Articles | Volume 17, issue 11
https://doi.org/10.5194/bg-17-2897-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-2897-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
03 Jun 2020
Research article |
| 03 Jun 2020
| 03 Jun 2020
Shell chemistry of the boreal Campanian bivalve Rastellum diluvianum (Linnaeus, 1767) reveals temperature seasonality, growth rates and life cycle of an extinct Cretaceous oyster
Niels J. de Winter
CORRESPONDING AUTHOR
AMGC research group, Vrije Universiteit Brussel, Pleinlaan 2, 1050
Brussels, Belgium
now at: Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, the Netherlands
Clemens V. Ullmann
Camborne School of Mines, University of Exeter, Penryn, Cornwall, TR10
9FE, UK
Anne M. Sørensen
Trap Danmark, Agem All 13, 2970, Hørsholm, Denmark
Nicolas Thibault
Department of Geoscience and Natural Resource Management, University
of Copenhagen, Øster Voldgade 10, 1350, Copenhagen, Denmark
Steven Goderis
AMGC research group, Vrije Universiteit Brussel, Pleinlaan 2, 1050
Brussels, Belgium
Stijn J. M. Van Malderen
A&MS research unit, Ghent University, Campus Sterre, Krijgslaan 281,
Building S12, 9000 Ghent, Belgium
Christophe Snoeck
AMGC research group, Vrije Universiteit Brussel, Pleinlaan 2, 1050
Brussels, Belgium
G-Time Laboratory, Université Libre de Bruxelles, 50 Avenue F.D. Roosevelt, 1050 Brussels, Belgium
Stijn Goolaerts
Directorate of Earth and History of Life, Royal Belgian Institute of
Natural Sciences, Vautierstraat 29, 1000 Brussels, Belgium
Frank Vanhaecke
A&MS research unit, Ghent University, Campus Sterre, Krijgslaan 281,
Building S12, 9000 Ghent, Belgium
Philippe Claeys
AMGC research group, Vrije Universiteit Brussel, Pleinlaan 2, 1050
Brussels, Belgium
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Mollusk shells are valuable recorders of climate and environmental changes of the past down to a daily resolution. To explore this potential, we measured changes in the composition of shells of two types of bivalves recorded at the hourly scale: the king scallop Pecten maximus and giant clams (Tridacna) that engaged in photosymbiosis. We find that photosymbiosis produces more day–night fluctuation in shell chemistry but that most of the variation is not periodic, perhaps recording weather.
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Matthias Sinnesael, Alfredo Loi, Marie-Pierre Dabard, Thijs R. A. Vandenbroucke, and Philippe Claeys
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Niels J. de Winter
Geosci. Model Dev., 15, 1247–1267, https://doi.org/10.5194/gmd-15-1247-2022, https://doi.org/10.5194/gmd-15-1247-2022, 2022
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ShellChron is a tool for determining the relative age of samples in carbonate (climate) archives based on the seasonal variability in temperature and salinity or precipitation recorded in stable oxygen isotope measurements. The model allows dating of fossil archives within a year, which is important for climate reconstructions on the sub-seasonal to decadal scale. In this paper, I introduce ShellChron and test it on a range of real and virtual datasets to demonstrate its use.
Thomas Munier, Jean-François Deconinck, Pierre Pellenard, Stephen P. Hesselbo, James B. Riding, Clemens V. Ullmann, Cédric Bougeault, Mathilde Mercuzot, Anne-Lise Santoni, Émilia Huret, and Philippe Landrein
Clim. Past, 17, 1547–1566, https://doi.org/10.5194/cp-17-1547-2021, https://doi.org/10.5194/cp-17-1547-2021, 2021
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Clay minerals are witnesses of alteration conditions in continental environments. Lacking high-resolution data on clay minerals, this work highlights wet and semi-arid cycles at mid-latitude in the upper Sinemurian. The higher proportion of kaolinite in the upper part of the obtusum zone and in the oxynotum zone indicates an increase in hydrolysis conditions in a warmer period confirmed by carbon isotopes.
Niels J. de Winter, Tobias Agterhuis, and Martin Ziegler
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Stef Vansteenberge, Niels J. de Winter, Matthias Sinnesael, Sophie Verheyden, Steven Goderis, Stijn J. M. Van Malderen, Frank Vanhaecke, and Philippe Claeys
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Flor Vermassen, Nanna Andreasen, David J. Wangner, Nicolas Thibault, Marit-Solveig Seidenkrantz, Rebecca Jackson, Sabine Schmidt, Kurt H. Kjær, and Camilla S. Andresen
Clim. Past, 15, 1171–1186, https://doi.org/10.5194/cp-15-1171-2019, https://doi.org/10.5194/cp-15-1171-2019, 2019
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Niels J. de Winter, Johan Vellekoop, Robin Vorsselmans, Asefeh Golreihan, Jeroen Soete, Sierra V. Petersen, Kyle W. Meyer, Silvio Casadio, Robert P. Speijer, and Philippe Claeys
Clim. Past, 14, 725–749, https://doi.org/10.5194/cp-14-725-2018, https://doi.org/10.5194/cp-14-725-2018, 2018
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In this work, we apply a range of methods to measure the geochemical composition of the calcite from fossil shells of Pycnodonte vesicularis (so-called honeycomb oysters). The goal is to investigate how the composition of these shells reflect the environment in which the animals grew. Ultimately, we propose a methodology to check whether the shells of pycnodonte oysters are well-preserved and to reconstruct meaningful information about the seasonal changes in the past climate and environment.
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Niels J. de Winter
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2017-137, https://doi.org/10.5194/gmd-2017-137, 2017
Revised manuscript not accepted
Short summary
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Bivalves grow by expanding their shells incrementally and record environmental conditions in the chemistry of their carbonate. To reconstruct these conditions, it is important to constrain the growth and trace element uptake rates in these bivalve shells. The present study models the development and chemical composition of the shells of bivalves based on XRF mapping of shell cross sections and allows changes in trace element uptake rates to be interpreted to reconstruct palaeoenvironment.
Clemens Vinzenz Ullmann and Philip A. E. Pogge von Strandmann
Biogeosciences, 14, 89–97, https://doi.org/10.5194/bg-14-89-2017, https://doi.org/10.5194/bg-14-89-2017, 2017
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This study documents how much control growth rate has on the chemical composition of fossil shell material. Using a series of chemical analyses of the fossil hard part of a belemnite, an extinct marine predator, a clear connection between the rate of calcite formation and its magnesium and strontium contents was found. These findings provide further insight into biomineralization processes and help better understand chemical signatures of fossils as proxies for palaeoenvironmental conditions.
Morgane Philippe, Jean-Louis Tison, Karen Fjøsne, Bryn Hubbard, Helle A. Kjær, Jan T. M. Lenaerts, Reinhard Drews, Simon G. Sheldon, Kevin De Bondt, Philippe Claeys, and Frank Pattyn
The Cryosphere, 10, 2501–2516, https://doi.org/10.5194/tc-10-2501-2016, https://doi.org/10.5194/tc-10-2501-2016, 2016
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The reconstruction of past snow accumulation rates is crucial in the context of recent climate change and sea level rise. We measured ~ 250 years of snow accumulation using a 120 m ice core drilled in coastal East Antarctica, where such long records are very scarce. This study is the first to show an increase in snow accumulation, beginning in the 20th and particularly marked in the last 50 years, thereby confirming model predictions of increased snowfall associated with climate change.
Sietske J. Batenburg, David De Vleeschouwer, Mario Sprovieri, Frederik J. Hilgen, Andrew S. Gale, Brad S. Singer, Christian Koeberl, Rodolfo Coccioni, Philippe Claeys, and Alessandro Montanari
Clim. Past, 12, 1995–2009, https://doi.org/10.5194/cp-12-1995-2016, https://doi.org/10.5194/cp-12-1995-2016, 2016
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The relative contributions of astronomical forcing and tectonics to ocean anoxia in the Cretaceous are unclear. This study establishes the pacing of Late Cretaceous black cherts and shales. We present a 6-million-year astrochronology from the Furlo and Bottaccione sections in Italy that spans the Cenomanian–Turonian transition and OAE2. Together with a new radioisotopic age for the mid-Cenomanian event, we show that astronomical forcing determined the timing of these carbon cycle perturbations.
Matthias Sinnesael, Miroslav Zivanovic, David De Vleeschouwer, Philippe Claeys, and Johan Schoukens
Geosci. Model Dev., 9, 3517–3531, https://doi.org/10.5194/gmd-9-3517-2016, https://doi.org/10.5194/gmd-9-3517-2016, 2016
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Classical spectral analysis often relies on methods based on (Fast) Fourier Transformation. This technique has no unique solution separating variations in amplitude and frequency. This drawback is circumvented by using a polynomial approach (ACE v.1 model) to estimate instantaneous amplitude and frequency in orbital components. The model is illustrated and validated using a synthetic insolation signal and tested on two case studies: a benthic δ18O record and a magnetic susceptibility record.
Stef Vansteenberge, Sophie Verheyden, Hai Cheng, R. Lawrence Edwards, Eddy Keppens, and Philippe Claeys
Clim. Past, 12, 1445–1458, https://doi.org/10.5194/cp-12-1445-2016, https://doi.org/10.5194/cp-12-1445-2016, 2016
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The use of stalagmites for last interglacial continental climate reconstructions in Europe has been successful in the past; however to expand the geographical coverage, additional data from Belgium is presented. It has been shown that stalagmite growth, morphology and stable isotope content reflect regional and local climate conditions, with Eemian optimum climate occurring between 125.3 and 117.3 ka. The start the Weichselian is expressed by a stop of growth caused by a drying climate.
Nicolas Thibault, Rikke Harlou, Niels H. Schovsbo, Lars Stemmerik, and Finn Surlyk
Clim. Past, 12, 429–438, https://doi.org/10.5194/cp-12-429-2016, https://doi.org/10.5194/cp-12-429-2016, 2016
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We present here for the first time a very high-resolution record of sea-surface temperature changes in the Boreal Chalk Sea for the last 8 million years of the Cretaceous. This record was obtained from 1932 bulk oxygen isotope measurements, and their interpretation into temperature trends is validated by similar trends observed from changes in phytoplankton assemblages.
C. Nehme, S. Verheyden, S. R. Noble, A. R. Farrant, D. Sahy, J. Hellstrom, J. J. Delannoy, and P. Claeys
Clim. Past, 11, 1785–1799, https://doi.org/10.5194/cp-11-1785-2015, https://doi.org/10.5194/cp-11-1785-2015, 2015
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The Levant is a key area to study palaeoclimatic responses over G-IG cycles. A precisely dated MIS 5 stalagmite (129–84ka) from Kanaan Cave, Lebanon, with growth rate and isotopic records variations indicate a warm humid phase at the last interglacial (~129-125ka). A shift in δ18O values (125-122ka) is driven by the source effect of the eastern Med. during sapropel 5 (S5). Low growth rates and high δ18O-δ13C values (~122-84ka) mark the onset of glacial inception and transition to drier phase.
M. Van Rampelbergh, S. Verheyden, M. Allan, Y. Quinif, H. Cheng, L. R. Edwards, E. Keppens, and P. Claeys
Clim. Past, 11, 789–802, https://doi.org/10.5194/cp-11-789-2015, https://doi.org/10.5194/cp-11-789-2015, 2015
M. Van Rampelbergh, S. Verheyden, M Allan, Y. Quinif, E. Keppens, and P. Claeys
Clim. Past, 10, 1871–1885, https://doi.org/10.5194/cp-10-1871-2014, https://doi.org/10.5194/cp-10-1871-2014, 2014
N. J. de Winter, C. Zeeden, and F. J. Hilgen
Clim. Past, 10, 1001–1015, https://doi.org/10.5194/cp-10-1001-2014, https://doi.org/10.5194/cp-10-1001-2014, 2014
Related subject area
Paleobiogeoscience: Marine Record
Ideas and perspectives: Human impacts alter the marine fossil record
Origin and role of non-skeletal carbonate in coralligenous build-ups: new geobiological perspectives in biomineralization processes
Serpulid microbialitic bioherms from the upper Sarmatian (Middle Miocene) of the central Paratethys Sea (NW Hungary) – witnesses of a microbial sea
Massive corals record deforestation in Malaysian Borneo through sediments in river discharge
Calcification response of planktic foraminifera to environmental change in the western Mediterranean Sea during the industrial era
Nature and origin of variations in pelagic carbonate production in the tropical ocean since the mid-Miocene (ODP Site 927)
Variation in calcification of Reticulofenestra coccoliths over the Oligocene–Early Miocene
The influence of near-surface sediment hydrothermalism on the TEX86 tetraether-lipid-based proxy and a new correction for ocean bottom lipid overprinting
Testing the effect of bioturbation and species abundance upon discrete-depth individual foraminifera analysis
Test-size evolution of the planktonic foraminifer Globorotalia menardii in the eastern tropical Atlantic since the Late Miocene
Distribution of coccoliths in surface sediments across the Drake Passage and calcification of Emiliania huxleyi morphotypes
Vertical distribution of planktic foraminifera through an oxygen minimum zone: how assemblages and test morphology reflect oxygen concentrations
Reconstructing past variations in environmental conditions and paleoproductivity over the last ∼ 8000 years off north-central Chile (30° S)
A 15-million-year-long record of phenotypic evolution in the heavily calcified coccolithophore Helicosphaera and its biogeochemical implications
Southern California margin benthic foraminiferal assemblages record recent centennial-scale changes in oxygen minimum zone
Baseline for ostracod-based northwestern Pacific and Indo-Pacific shallow-marine paleoenvironmental reconstructions: ecological modeling of species distributions
Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia)
Coastal primary productivity changes over the last millennium: a case study from the Skagerrak (North Sea)
A 1500-year multiproxy record of coastal hypoxia from the northern Baltic Sea indicates unprecedented deoxygenation over the 20th century
Technical note: An empirical method for absolute calibration of coccolith thickness
Reconstructing Holocene temperature and salinity variations in the western Baltic Sea region: a multi-proxy comparison from the Little Belt (IODP Expedition 347, Site M0059)
The oxic degradation of sedimentary organic matter 1400 Ma constrains atmospheric oxygen levels
Geochemical and microstructural characterisation of two species of cool-water bivalves (Fulvia tenuicostata and Soletellina biradiata) from Western Australia
Ecological response to collapse of the biological pump following the mass extinction at the Cretaceous–Paleogene boundary
Quantifying the Cenozoic marine diatom deposition history: links to the C and Si cycles
Anthropogenically induced environmental changes in the northeastern Adriatic Sea in the last 500 years (Panzano Bay, Gulf of Trieste)
Palaeohydrological changes over the last 50 ky in the central Gulf of Cadiz: complex forcing mechanisms mixing multi-scale processes
Dinocyst assemblage constraints on oceanographic and atmospheric processes in the eastern equatorial Atlantic over the last 44 kyr
Sedimentary response to sea ice and atmospheric variability over the instrumental period off Adélie Land, East Antarctica
Equatorward phytoplankton migration during a cold spell within the Late Cretaceous super-greenhouse
Upwellings mitigated Plio-Pleistocene heat stress for reef corals on the Florida platform (USA)
Millennial changes in North Atlantic oxygen concentrations
Vanishing coccolith vital effects with alleviated carbon limitation
Late Pleistocene glacial–interglacial shell-size–isotope variability in planktonic foraminifera as a function of local hydrography
Coral records of reef-water pH across the central Great Barrier Reef, Australia: assessing the influence of river runoff on inshore reefs
Records of past mid-depth ventilation: Cretaceous ocean anoxic event 2 vs. Recent oxygen minimum zones
Organomineral nanocomposite carbon burial during Oceanic Anoxic Event 2
Non-invasive imaging methods applied to neo- and paleo-ontological cephalopod research
Icehouse–greenhouse variations in marine denitrification
Changes in calcification of coccoliths under stable atmospheric CO2
Southern Hemisphere imprint for Indo-Asian summer monsoons during the last glacial period as revealed by Arabian Sea productivity records
The calcareous nannofossil Prinsiosphaera achieved rock-forming abundances in the latest Triassic of western Tethys: consequences for the δ13C of bulk carbonate
The Little Ice Age: evidence from a sediment record in Gullmar Fjord, Swedish west coast
Nitrogen isotopes in bulk marine sediment: linking seafloor observations with subseafloor records
Quantitative reconstruction of sea-surface conditions over the last 150 yr in the Beaufort Sea based on dinoflagellate cyst assemblages: the role of large-scale atmospheric circulation patterns
Spatial linkages between coral proxies of terrestrial runoff across a large embayment in Madagascar
Pteropods from the Caribbean Sea: variations in calcification as an indicator of past ocean carbonate saturation
Sedimentary organic matter and carbonate variations in the Chukchi Borderland in association with ice sheet and ocean-atmosphere dynamics over the last 155 kyr
First discovery of dolomite and magnesite in living coralline algae and its geobiological implications
Assessment of sea surface temperature changes in the Gulf of Cadiz during the last 30 ka: implications for glacial changes in the regional hydrography
Rafał Nawrot, Martin Zuschin, Adam Tomašových, Michał Kowalewski, and Daniele Scarponi
EGUsphere, https://doi.org/10.5194/egusphere-2023-2974, https://doi.org/10.5194/egusphere-2023-2974, 2024
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The youngest fossil record is a crucial source of data on the history of marine ecosystems and their long-term alteration by humans. However, human activities that reshape ecosystems also alter sedimentary and biological processes that control the formation of the geological archives recording those impacts. Thus, humans have been transforming the marine fossil record in ways that affect our ability to reconstruct past ecological and climate dynamics.
Mara Cipriani, Carmine Apollaro, Daniela Basso, Pietro Bazzicalupo, Marco Bertolino, Valentina Alice Bracchi, Fabio Bruno, Gabriele Costa, Rocco Dominici, Alessandro Gallo, Maurizio Muzzupappa, Antonietta Rosso, Rossana Sanfilippo, Francesco Sciuto, Giovanni Vespasiano, and Adriano Guido
Biogeosciences, 21, 49–72, https://doi.org/10.5194/bg-21-49-2024, https://doi.org/10.5194/bg-21-49-2024, 2024
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Who constructs the build-ups of the Mediterranean Sea? What is the role of skeletal and soft-bodied organisms in these bioconstructions? Do bacteria play a role in their formation? In this research, for the first time, the coralligenous of the Mediterranean shelf is studied from a geobiological point of view with an interdisciplinary biological and geological approach, highlighting important biotic relationships that can be used in interpreting the fossil build-up systems.
Mathias Harzhauser, Oleg Mandic, and Werner E. Piller
Biogeosciences, 20, 4775–4794, https://doi.org/10.5194/bg-20-4775-2023, https://doi.org/10.5194/bg-20-4775-2023, 2023
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Bowl-shaped spirorbid microbialite bioherms formed during the late Middle Miocene (Sarmatian) in the central Paratethys Sea under a warm, arid climate. The microbialites and the surrounding sediment document a predominance of microbial activity in the shallow marine environments of the sea at that time. Modern microbialites are not analogues for these unique structures, which reflect a series of growth stages with an initial “start-up stage”, massive “keep-up stage” and termination of growth.
Walid Naciri, Arnoud Boom, Matthew Payne, Nicola Browne, Noreen J. Evans, Philip Holdship, Kai Rankenburg, Ramasamy Nagarajan, Bradley J. McDonald, Jennifer McIlwain, and Jens Zinke
Biogeosciences, 20, 1587–1604, https://doi.org/10.5194/bg-20-1587-2023, https://doi.org/10.5194/bg-20-1587-2023, 2023
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In this study, we tested the ability of massive boulder-like corals to act as archives of land use in Malaysian Borneo to palliate the lack of accurate instrumental data on deforestation before the 1980s. We used mass spectrometry to measure trace element ratios in coral cores to use as a proxy for sediment in river discharge. Results showed an extremely similar increase between our proxy and the river discharge instrumental record, demonstrating the use of these corals as reliable archives.
Thibauld M. Béjard, Andrés S. Rigual-Hernández, José A. Flores, Javier P. Tarruella, Xavier Durrieu de Madron, Isabel Cacho, Neghar Haghipour, Aidan Hunter, and Francisco J. Sierro
Biogeosciences, 20, 1505–1528, https://doi.org/10.5194/bg-20-1505-2023, https://doi.org/10.5194/bg-20-1505-2023, 2023
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The Mediterranean Sea is undergoing a rapid and unprecedented environmental change. Planktic foraminifera calcification is affected on different timescales. On seasonal and interannual scales, calcification trends differ according to the species and are linked mainly to sea surface temperatures and carbonate system parameters, while comparison with pre/post-industrial assemblages shows that all three species have reduced their calcification between 10 % to 35 % according to the species.
Pauline Cornuault, Thomas Westerhold, Heiko Pälike, Torsten Bickert, Karl-Heinz Baumann, and Michal Kucera
Biogeosciences, 20, 597–618, https://doi.org/10.5194/bg-20-597-2023, https://doi.org/10.5194/bg-20-597-2023, 2023
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We generated high-resolution records of carbonate accumulation rate from the Miocene to the Quaternary in the tropical Atlantic Ocean to characterize the variability in pelagic carbonate production during warm climates. It follows orbital cycles, responding to local changes in tropical conditions, as well as to long-term shifts in climate and ocean chemistry. These changes were sufficiently large to play a role in the carbon cycle and global climate evolution.
José Guitián, Miguel Ángel Fuertes, José-Abel Flores, Iván Hernández-Almeida, and Heather Stoll
Biogeosciences, 19, 5007–5019, https://doi.org/10.5194/bg-19-5007-2022, https://doi.org/10.5194/bg-19-5007-2022, 2022
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The effect of environmental conditions on the degree of calcification of marine phytoplankton remains unclear. This study implements a new microscopic approach to quantify the calcification of ancient coccolithophores, using North Atlantic sediments. Results show significant differences in the thickness and shape factor of coccoliths for samples with minimum dissolution, providing the first evaluation of phytoplankton physiology adaptation to million-year-scale variable environmental conditions.
Jeremy N. Bentley, Gregory T. Ventura, Clifford C. Walters, Stefan M. Sievert, and Jeffrey S. Seewald
Biogeosciences, 19, 4459–4477, https://doi.org/10.5194/bg-19-4459-2022, https://doi.org/10.5194/bg-19-4459-2022, 2022
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We demonstrate the TEX86 (TetraEther indeX of 86 carbon atoms) paleoclimate proxy can become heavily impacted by the ocean floor archaeal community. The impact results from source inputs, their diagenetic and catagenetic alteration, and further overprint by the additions of lipids from the ocean floor sedimentary archaeal community. We then present a method to correct the overprints by using IPLs (intact polar lipids) extracted from both water column and subsurface archaeal communities.
Bryan C. Lougheed and Brett Metcalfe
Biogeosciences, 19, 1195–1209, https://doi.org/10.5194/bg-19-1195-2022, https://doi.org/10.5194/bg-19-1195-2022, 2022
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Measurements on sea-dwelling shelled organisms called foraminifera retrieved from deep-sea sediment cores have been used to reconstruct sea surface temperature (SST) variation. To evaluate the method, we use a computer model to simulate millions of single foraminifera and how they become mixed in the sediment after being deposited on the seafloor. We compare the SST inferred from the single foraminifera in the sediment core to the true SST in the water, thus quantifying method uncertainties.
Thore Friesenhagen
Biogeosciences, 19, 777–805, https://doi.org/10.5194/bg-19-777-2022, https://doi.org/10.5194/bg-19-777-2022, 2022
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Size measurements of the planktonic foraminifer Globorotalia menardii and related forms are used to investigate the shell-size evolution for the last 8 million years in the eastern tropical Atlantic Ocean. Long-term changes in the shell size coincide with major climatic, palaeogeographic and palaeoceanographic changes and suggest the occurrence of a new G. menardii type in the Atlantic Ocean ca. 2 million years ago.
Nele Manon Vollmar, Karl-Heinz Baumann, Mariem Saavedra-Pellitero, and Iván Hernández-Almeida
Biogeosciences, 19, 585–612, https://doi.org/10.5194/bg-19-585-2022, https://doi.org/10.5194/bg-19-585-2022, 2022
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We studied recent (sub-)fossil remains of a type of algae (coccolithophores) off southernmost Chile and across the Drake Passage, adding to the scarce knowledge that exists in the Southern Ocean, a rapidly changing environment. We found that those can be used to reconstruct the surface ocean conditions in the north but not in the south. We also found variations in shape in the dominant species Emiliania huxleyi depending on the location, indicating subtle adaptations to environmental conditions.
Catherine V. Davis, Karen Wishner, Willem Renema, and Pincelli M. Hull
Biogeosciences, 18, 977–992, https://doi.org/10.5194/bg-18-977-2021, https://doi.org/10.5194/bg-18-977-2021, 2021
Práxedes Muñoz, Lorena Rebolledo, Laurent Dezileau, Antonio Maldonado, Christoph Mayr, Paola Cárdenas, Carina B. Lange, Katherine Lalangui, Gloria Sanchez, Marco Salamanca, Karen Araya, Ignacio Jara, Gabriel Easton, and Marcel Ramos
Biogeosciences, 17, 5763–5785, https://doi.org/10.5194/bg-17-5763-2020, https://doi.org/10.5194/bg-17-5763-2020, 2020
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We analyze marine sedimentary records to study temporal changes in oxygen and productivity in marine waters of central Chile. We observed increasing oxygenation and decreasing productivity from 6000 kyr ago to the modern era that seem to respond to El Niño–Southern Oscillation activity. In the past centuries, deoxygenation and higher productivity are re-established, mainly in the northern zones of Chile and Peru. Meanwhile, in north-central Chile the deoxygenation trend is maintained.
Luka Šupraha and Jorijntje Henderiks
Biogeosciences, 17, 2955–2969, https://doi.org/10.5194/bg-17-2955-2020, https://doi.org/10.5194/bg-17-2955-2020, 2020
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The cell size, degree of calcification and growth rates of coccolithophores impact their role in the carbon cycle and may also influence their adaptation to environmental change. Combining insights from culture experiments and the fossil record, we show that the selection for smaller cells over the past 15 Myr has been a common adaptive trait among different lineages. However, heavily calcified species maintained a more stable biogeochemical output than the ancestral lineage of E. huxleyi.
Hannah M. Palmer, Tessa M. Hill, Peter D. Roopnarine, Sarah E. Myhre, Katherine R. Reyes, and Jonas T. Donnenfield
Biogeosciences, 17, 2923–2937, https://doi.org/10.5194/bg-17-2923-2020, https://doi.org/10.5194/bg-17-2923-2020, 2020
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Modern climate change is causing expansions of low-oxygen zones, with detrimental impacts to marine life. To better predict future ocean oxygen change, we study past expansions and contractions of low-oxygen zones using microfossils of seafloor organisms. We find that, along the San Diego margin, the low-oxygen zone expanded into more shallow water in the last 400 years, but the conditions within and below the low-oxygen zone did not change significantly in the last 1500 years.
Yuanyuan Hong, Moriaki Yasuhara, Hokuto Iwatani, and Briony Mamo
Biogeosciences, 16, 585–604, https://doi.org/10.5194/bg-16-585-2019, https://doi.org/10.5194/bg-16-585-2019, 2019
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This study analyzed microfaunal assemblages in surface sediments from 52 sites in Hong Kong marine waters. We selected 18 species for linear regression modeling to statistically reveal the relationship between species distribution and environmental factors. These results show environmental preferences of commonly distributed species on Asian coasts, providing a robust baseline for past environmental reconstruction of the broad Asian region using microfossils in sediment cores.
Jorge Domingo Carrillo-Briceño, Zoneibe Luz, Austin Hendy, László Kocsis, Orangel Aguilera, and Torsten Vennemann
Biogeosciences, 16, 33–56, https://doi.org/10.5194/bg-16-33-2019, https://doi.org/10.5194/bg-16-33-2019, 2019
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By combining taxonomy and geochemistry, we corroborated the described paleoenvironments from a Neogene fossiliferous deposit of South America. Shark teeth specimens were used for taxonomic identification and as proxies for geochemical analyses. With a multidisciplinary approach we refined the understanding about the paleoenvironmental setting and the paleoecological characteristics of the studied groups, in our case, for the bull shark and its incursions into brackish waters.
Anna Binczewska, Bjørg Risebrobakken, Irina Polovodova Asteman, Matthias Moros, Amandine Tisserand, Eystein Jansen, and Andrzej Witkowski
Biogeosciences, 15, 5909–5928, https://doi.org/10.5194/bg-15-5909-2018, https://doi.org/10.5194/bg-15-5909-2018, 2018
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Primary productivity is an important factor in the functioning and structuring of the coastal ecosystem. Thus, two sediment cores from the Skagerrak (North Sea) were investigated in order to obtain a comprehensive picture of primary productivity changes during the last millennium and identify associated forcing factors (e.g. anthropogenic, climate). The cores were dated and analysed for palaeoproductivity proxies and palaeothermometers.
Sami A. Jokinen, Joonas J. Virtasalo, Tom Jilbert, Jérôme Kaiser, Olaf Dellwig, Helge W. Arz, Jari Hänninen, Laura Arppe, Miia Collander, and Timo Saarinen
Biogeosciences, 15, 3975–4001, https://doi.org/10.5194/bg-15-3975-2018, https://doi.org/10.5194/bg-15-3975-2018, 2018
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Oxygen deficiency is a major environmental problem deteriorating seafloor habitats especially in the coastal ocean with large human impact. Here we apply a wide set of chemical and physical analyses to a 1500-year long sediment record and show that, although long-term climate variability has modulated seafloor oxygenation in the coastal northern Baltic Sea, the oxygen loss over the 20th century is unprecedentedly severe, emphasizing the need to reduce anthropogenic nutrient input in the future.
Saúl González-Lemos, José Guitián, Miguel-Ángel Fuertes, José-Abel Flores, and Heather M. Stoll
Biogeosciences, 15, 1079–1091, https://doi.org/10.5194/bg-15-1079-2018, https://doi.org/10.5194/bg-15-1079-2018, 2018
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Changes in atmospheric carbon dioxide affect ocean chemistry and the ability of marine organisms to manufacture shells from calcium carbonate. We describe a technique to obtain more reproducible measurements of the thickness of calcium carbonate shells made by microscopic marine algae called coccolithophores, which will allow researchers to compare how the shell thickness responds to variations in ocean chemistry in the past and present.
Ulrich Kotthoff, Jeroen Groeneveld, Jeanine L. Ash, Anne-Sophie Fanget, Nadine Quintana Krupinski, Odile Peyron, Anna Stepanova, Jonathan Warnock, Niels A. G. M. Van Helmond, Benjamin H. Passey, Ole Rønø Clausen, Ole Bennike, Elinor Andrén, Wojciech Granoszewski, Thomas Andrén, Helena L. Filipsson, Marit-Solveig Seidenkrantz, Caroline P. Slomp, and Thorsten Bauersachs
Biogeosciences, 14, 5607–5632, https://doi.org/10.5194/bg-14-5607-2017, https://doi.org/10.5194/bg-14-5607-2017, 2017
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We present reconstructions of paleotemperature, paleosalinity, and paleoecology from the Little Belt (Site M0059) over the past ~ 8000 years and evaluate the applicability of numerous proxies. Conditions were lacustrine until ~ 7400 cal yr BP. A transition to brackish–marine conditions then occurred within ~ 200 years. Salinity proxies rarely allowed quantitative estimates but revealed congruent results, while quantitative temperature reconstructions differed depending on the proxies used.
Shuichang Zhang, Xiaomei Wang, Huajian Wang, Emma U. Hammarlund, Jin Su, Yu Wang, and Donald E. Canfield
Biogeosciences, 14, 2133–2149, https://doi.org/10.5194/bg-14-2133-2017, https://doi.org/10.5194/bg-14-2133-2017, 2017
Liza M. Roger, Annette D. George, Jeremy Shaw, Robert D. Hart, Malcolm Roberts, Thomas Becker, Bradley J. McDonald, and Noreen J. Evans
Biogeosciences, 14, 1721–1737, https://doi.org/10.5194/bg-14-1721-2017, https://doi.org/10.5194/bg-14-1721-2017, 2017
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The shell compositions of bivalve species from south Western Australia are described here to better understand the factors involved in their formation. The shell composition can be used to reconstruct past environmental conditions, but certain species manifest an offset compared to the environmental parameters measured. As shown here, shells that experience the same conditions can present different compositions in relation to structure, organic composition and environmental conditions.
Johan Vellekoop, Lineke Woelders, Sanem Açikalin, Jan Smit, Bas van de Schootbrugge, Ismail Ö. Yilmaz, Henk Brinkhuis, and Robert P. Speijer
Biogeosciences, 14, 885–900, https://doi.org/10.5194/bg-14-885-2017, https://doi.org/10.5194/bg-14-885-2017, 2017
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The Cretaceous–Paleogene boundary, ~ 66 Ma, is characterized by a mass extinction. We studied groups of both surface-dwelling and bottom-dwelling organisms to unravel the oceanographic consequences of these extinctions. Our integrated records indicate that a reduction of the transport of organic matter to the sea floor resulted in enhanced recycling of nutrients in the upper water column and decreased food supply at the sea floor in the first tens of thousands of years after the extinctions.
Johan Renaudie
Biogeosciences, 13, 6003–6014, https://doi.org/10.5194/bg-13-6003-2016, https://doi.org/10.5194/bg-13-6003-2016, 2016
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Marine planktonic diatoms are today both the main silica and carbon exporter to the deep sea. However, 50 million years ago, radiolarians were the main silica exporter and diatoms were a rare, geographically restricted group. Quantification of their rise to dominance suggest that diatom abundance is primarily controlled by the continental weathering and has a negative feedback, observable on a geological timescale, on the carbon cycle.
Jelena Vidović, Rafał Nawrot, Ivo Gallmetzer, Alexandra Haselmair, Adam Tomašových, Michael Stachowitsch, Vlasta Ćosović, and Martin Zuschin
Biogeosciences, 13, 5965–5981, https://doi.org/10.5194/bg-13-5965-2016, https://doi.org/10.5194/bg-13-5965-2016, 2016
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We studied the ecological history of the Gulf of Trieste. Before the 20th century, the only activity here was ore mining, releasing high amounts of mercury into its northern part, Panzano Bay. Mercury did not cause changes to microorganisms, as it is not bioavailable. In the 20th century, agriculture caused nutrient enrichment in the bay and increased diversity of microorganisms. Industrial activities increased the concentrations of pollutants, causing only minor changes to microorganisms.
Aurélie Penaud, Frédérique Eynaud, Antje Helga Luise Voelker, and Jean-Louis Turon
Biogeosciences, 13, 5357–5377, https://doi.org/10.5194/bg-13-5357-2016, https://doi.org/10.5194/bg-13-5357-2016, 2016
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This paper presents new analyses conducted at high resolution in the Gulf of Cadiz over the last 50 ky. Palaeohydrological changes in these subtropical latitudes are discussed through dinoflagellate cyst assemblages but also dinocyst transfer function results, implying sea surface temperature and salinity as well as annual productivity reconstructions. This study is thus important for our understanding of past and future productivity regimes, also implying consequences on the biological pump.
William Hardy, Aurélie Penaud, Fabienne Marret, Germain Bayon, Tania Marsset, and Laurence Droz
Biogeosciences, 13, 4823–4841, https://doi.org/10.5194/bg-13-4823-2016, https://doi.org/10.5194/bg-13-4823-2016, 2016
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Our approach is based on a multi-proxy study from a core collected off the Congo River and discusses surface oceanic conditions (upwelling cells, river-induced upwelling), land–sea interactions and terrestrial erosion and in particular enables us to spatially constrain the migration of atmospheric systems. This paper thus presents new data highlighting, with the highest resolution ever reached in this region, the great correlation between phytoplanktonic organisms and monsoonal mechanisms.
Philippine Campagne, Xavier Crosta, Sabine Schmidt, Marie Noëlle Houssais, Olivier Ther, and Guillaume Massé
Biogeosciences, 13, 4205–4218, https://doi.org/10.5194/bg-13-4205-2016, https://doi.org/10.5194/bg-13-4205-2016, 2016
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Diatoms and biomarkers have been recently used for palaeoclimate reconstructions in the Southern Ocean. Few sediment-based ecological studies have investigated their relationships with environmental conditions. Here, we compare high-resolution sedimentary records with meteorological data to study relationships between our proxies and recent atmospheric and sea surface changes. Our results indicate that coupled wind pattern and sea surface variability act as the proximal forcing at that scale.
Niels A. G. M. van Helmond, Appy Sluijs, Nina M. Papadomanolaki, A. Guy Plint, Darren R. Gröcke, Martin A. Pearce, James S. Eldrett, João Trabucho-Alexandre, Ireneusz Walaszczyk, Bas van de Schootbrugge, and Henk Brinkhuis
Biogeosciences, 13, 2859–2872, https://doi.org/10.5194/bg-13-2859-2016, https://doi.org/10.5194/bg-13-2859-2016, 2016
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Over the past decades large changes have been observed in the biogeographical dispersion of marine life resulting from climate change. To better understand present and future trends it is important to document and fully understand the biogeographical response of marine life during episodes of environmental change in the geological past.
Here we investigate the response of phytoplankton, the base of the marine food web, to a rapid cold spell, interrupting greenhouse conditions during the Cretaceous.
Thomas C. Brachert, Markus Reuter, Stefan Krüger, Julia Kirkerowicz, and James S. Klaus
Biogeosciences, 13, 1469–1489, https://doi.org/10.5194/bg-13-1469-2016, https://doi.org/10.5194/bg-13-1469-2016, 2016
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We present stable isotope proxy data and calcification records from fossil reef corals. The corals investigated derive from the Florida carbonate platform and are of middle Pliocene to early Pleistocene age. From the data we infer an environment subject to intermittent upwelling on annual to decadal timescales. Calcification rates were enhanced during periods of upwelling. This is likely an effect of dampened SSTs during the upwelling.
B. A. A. Hoogakker, D. J. R. Thornalley, and S. Barker
Biogeosciences, 13, 211–221, https://doi.org/10.5194/bg-13-211-2016, https://doi.org/10.5194/bg-13-211-2016, 2016
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Models predict a decrease in future ocean O2, driven by surface water warming and freshening in the polar regions, causing a reduction in ocean circulation. Here we assess this effect in the past, focussing on the response of deep and intermediate waters from the North Atlantic during large-scale ice rafting and millennial-scale cooling events of the last glacial.
Our assessment agrees with the models but also highlights the importance of biological processes driving ocean O2 change.
M. Hermoso, I. Z. X. Chan, H. L. O. McClelland, A. M. C. Heureux, and R. E. M. Rickaby
Biogeosciences, 13, 301–312, https://doi.org/10.5194/bg-13-301-2016, https://doi.org/10.5194/bg-13-301-2016, 2016
B. Metcalfe, W. Feldmeijer, M. de Vringer-Picon, G.-J. A. Brummer, F. J. C. Peeters, and G. M. Ganssen
Biogeosciences, 12, 4781–4807, https://doi.org/10.5194/bg-12-4781-2015, https://doi.org/10.5194/bg-12-4781-2015, 2015
Short summary
Short summary
Iron biogeochemical budgets during the natural ocean fertilisation experiment KEOPS-2 showed that complex circulation and transport pathways were responsible for differences in the mode and strength of iron supply, with vertical supply dominant on the plateau and lateral supply dominant in the plume. The exchange of iron between dissolved, biogenic and lithogenic pools was highly dynamic, resulting in a decoupling of iron supply and carbon export and controlling the efficiency of fertilisation.
J. P. D'Olivo, M. T. McCulloch, S. M. Eggins, and J. Trotter
Biogeosciences, 12, 1223–1236, https://doi.org/10.5194/bg-12-1223-2015, https://doi.org/10.5194/bg-12-1223-2015, 2015
Short summary
Short summary
The boron isotope composition in the skeleton of massive Porites corals from the central Great Barrier Reef is used to reconstruct the seawater pH over the 1940-2009 period. The long-term decline in the coral-reconstructed seawater pH is in close agreement with estimates based on the CO2 uptake by surface waters due to rising atmospheric levels. We also observed a significant relationship between terrestrial runoff data and the inshore coral boron isotopes records.
J. Schönfeld, W. Kuhnt, Z. Erdem, S. Flögel, N. Glock, M. Aquit, M. Frank, and A. Holbourn
Biogeosciences, 12, 1169–1189, https://doi.org/10.5194/bg-12-1169-2015, https://doi.org/10.5194/bg-12-1169-2015, 2015
Short summary
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Today’s oceans show distinct mid-depth oxygen minima while whole oceanic basins became transiently anoxic in the Mesozoic. To constrain past bottom-water oxygenation, we compared sediments from the Peruvian OMZ with the Cenomanian OAE 2 from Morocco. Corg accumulation rates in laminated OAE 2 sections match Holocene rates off Peru. Laminated deposits are found at oxygen levels of < 7µmol kg-1; crab burrows appear at 10µmol kg-1 today, both defining threshold values for palaeoreconstructions.
S. C. Löhr and M. J. Kennedy
Biogeosciences, 11, 4971–4983, https://doi.org/10.5194/bg-11-4971-2014, https://doi.org/10.5194/bg-11-4971-2014, 2014
R. Hoffmann, J. A. Schultz, R. Schellhorn, E. Rybacki, H. Keupp, S. R. Gerden, R. Lemanis, and S. Zachow
Biogeosciences, 11, 2721–2739, https://doi.org/10.5194/bg-11-2721-2014, https://doi.org/10.5194/bg-11-2721-2014, 2014
T. J. Algeo, P. A. Meyers, R. S. Robinson, H. Rowe, and G. Q. Jiang
Biogeosciences, 11, 1273–1295, https://doi.org/10.5194/bg-11-1273-2014, https://doi.org/10.5194/bg-11-1273-2014, 2014
C. Berger, K. J. S. Meier, H. Kinkel, and K.-H. Baumann
Biogeosciences, 11, 929–944, https://doi.org/10.5194/bg-11-929-2014, https://doi.org/10.5194/bg-11-929-2014, 2014
T. Caley, S. Zaragosi, J. Bourget, P. Martinez, B. Malaizé, F. Eynaud, L. Rossignol, T. Garlan, and N. Ellouz-Zimmermann
Biogeosciences, 10, 7347–7359, https://doi.org/10.5194/bg-10-7347-2013, https://doi.org/10.5194/bg-10-7347-2013, 2013
N. Preto, C. Agnini, M. Rigo, M. Sprovieri, and H. Westphal
Biogeosciences, 10, 6053–6068, https://doi.org/10.5194/bg-10-6053-2013, https://doi.org/10.5194/bg-10-6053-2013, 2013
I. Polovodova Asteman, K. Nordberg, and H. L. Filipsson
Biogeosciences, 10, 1275–1290, https://doi.org/10.5194/bg-10-1275-2013, https://doi.org/10.5194/bg-10-1275-2013, 2013
J.-E. Tesdal, E. D. Galbraith, and M. Kienast
Biogeosciences, 10, 101–118, https://doi.org/10.5194/bg-10-101-2013, https://doi.org/10.5194/bg-10-101-2013, 2013
L. Durantou, A. Rochon, D. Ledu, G. Massé, S. Schmidt, and M. Babin
Biogeosciences, 9, 5391–5406, https://doi.org/10.5194/bg-9-5391-2012, https://doi.org/10.5194/bg-9-5391-2012, 2012
C. A. Grove, J. Zinke, T. Scheufen, J. Maina, E. Epping, W. Boer, B. Randriamanantsoa, and G.-J. A. Brummer
Biogeosciences, 9, 3063–3081, https://doi.org/10.5194/bg-9-3063-2012, https://doi.org/10.5194/bg-9-3063-2012, 2012
D. Wall-Palmer, M. B. Hart, C. W. Smart, R. S. J. Sparks, A. Le Friant, G. Boudon, C. Deplus, and J. C. Komorowski
Biogeosciences, 9, 309–315, https://doi.org/10.5194/bg-9-309-2012, https://doi.org/10.5194/bg-9-309-2012, 2012
S. F. Rella and M. Uchida
Biogeosciences, 8, 3545–3553, https://doi.org/10.5194/bg-8-3545-2011, https://doi.org/10.5194/bg-8-3545-2011, 2011
M. C. Nash, U. Troitzsch, B. N. Opdyke, J. M. Trafford, B. D. Russell, and D. I. Kline
Biogeosciences, 8, 3331–3340, https://doi.org/10.5194/bg-8-3331-2011, https://doi.org/10.5194/bg-8-3331-2011, 2011
A. Penaud, F. Eynaud, A. Voelker, M. Kageyama, F. Marret, J. L. Turon, D. Blamart, T. Mulder, and L. Rossignol
Biogeosciences, 8, 2295–2316, https://doi.org/10.5194/bg-8-2295-2011, https://doi.org/10.5194/bg-8-2295-2011, 2011
Cited articles
Al-Aasm, I. S. and Veizer, J.: Diagenetic stabilization of aragonite and
low-Mg calcite, II. Stable isotopes in rudists, J. Sediment.
Res., 56, 763–770, 1986a.
Al-Aasm, I. S. and Veizer, J.: Diagenetic stabilization of aragonite and
low-Mg calcite, I. Trace elements in rudists, J. Sediment.
Res., 56, 138–152, 1986b.
Alberti, M., Fürsich, F. T., Abdelhady, A. A., and Andersen, N.: Middle
to Late Jurassic equatorial seawater temperatures and latitudinal
temperature gradients based on stable isotopes of brachiopods and oysters
from Gebel Maghara, Egypt, Palaeogeogr. Palaeocl., 468, 301–313, https://doi.org/10.1016/j.palaeo.2016.11.052, 2017.
Amiot, R., Lécuyer, C., Buffetaut, E., Fluteau, F., Legendre, S., and
Martineau, F.: Latitudinal temperature gradient during the Cretaceous Upper
Campanian–Middle Maastrichtian: δ18O record of continental
vertebrates, Earth Planet. Sc. Lett., 226, 255–272,
https://doi.org/10.1016/j.epsl.2004.07.015, 2004.
Andreasson, F. P. and Schmitz, B.: Winter and summer temperatures of the
early middle Eocene of France from Turritella δ18O profiles, Geology, 4, 1067–1070, 1996.
Arthur, M. A., Williams, D. F., and Jones, D. S.: Seasonal
temperature-salinity changes and thermocline development in the mid-Atlantic
Bight as recorded by the isotopic composition of bivalves, Geology, 11,
655–659, https://doi.org/10.1130/0091-7613(1983)11<655:STCATD>2.0.CO;2, 1983.
Bachelet, G.: Growth and recruitment of the tellinid bivalve Macoma balthica
at the southern limit of its geographical distribution, the Gironde estuary
(SW France), Mar. Biol., 59, 105–117, 1980.
Barlow, R.: Asymmetric systematic errors, arXiv [preprint], arXiv:0306138, 18 June 2003.
Barrera, E. and Johnson, C. C.: Evolution of the Cretaceous Ocean-climate
System, Geol. Soc. Am., 332, 1–419, 1999.
Berthelin, C., Kellner, K., and Mathieu, M.: Storage metabolism in the
Pacific oyster (Crassostrea gigas) in relation to summer mortalities and
reproductive cycle (West Coast of France), Comp. Biochem.
Phys. B, 125, 359–369,
https://doi.org/10.1016/S0305-0491(99)00187-X, 2000.
Brand, U. and Veizer, J.: Chemical diagenesis of a multicomponent carbonate
system – 1: Trace elements, J. Sediment. Res., 50,
1219–1236, 1980.
Brand, U. and Veizer, J.: Chemical diagenesis of a multicomponent carbonate
system-2: stable isotopes, J. Sediment. Res., 51, 987–997,
1981.
Bryan, S. P. and Marchitto, T. M.: Mg∕Ca – temperature proxy in benthic
foraminifera: New calibrations from the Florida Straits and a hypothesis
regarding Mg∕Li, Paleoceanography, 23, PA2220, https://doi.org/10.1029/2007PA001553,
2008.
Burgener, L., Hyland, E., Huntington, K. W., Kelson, J. R., and Sewall, J.
O.: Revisiting the equable climate problem during the Late Cretaceous
greenhouse using paleosol carbonate clumped isotope temperatures from the
Campanian of the Western Interior Basin, USA, Palaeogeogr.,
Palaeocl., 516, 244–267,
https://doi.org/10.1016/j.palaeo.2018.12.004, 2018.
Butler, P. G., Wanamaker, A. D., Scourse, J. D., Richardson, C. A., and
Reynolds, D. J.: Variability of marine climate on the North Icelandic Shelf
in a 1357-year proxy archive based on growth increments in the bivalve
Arctica islandica, Palaeogeogr. Palaeocl., 373,
141–151, https://doi.org/10.1016/j.palaeo.2012.01.016, 2013.
Carriker, M. R., Palmer, R. E., and Prezant, R. S.: Functional
ultramorphology of the dissoconch valves of the oyster Crassostrea
virginica, in: Proceedings of the National Shellfisheries Association, Vol.
70, 139–183, 1979.
Carriker, M. R., Swann, C. P., Prezant, R. S., and Counts, C. L.: Chemical
elements in the aragonitic and calcitic microstructural groups of shell of
the oysterCrassostrea virginica: A proton probe study, Mar. Biol.,
109, 287–297, 1991.
Chauvaud, L., Thébault, J., Clavier, J., Lorrain, A., and Strand, Ø.:
What's Hiding Behind Ontogenetic δ13C Variations in Mollusk Shells?
New Insights from the Great Scallop (Pecten maximus), Estuar. Coast.,
34, 211–220, https://doi.org/10.1007/s12237-010-9267-4, 2011.
Christensen, W. K.: Upper Cretaceous belemnites from the Kristianstad area
in Scania, Fossils and Strata, 7, 1–70, 1975.
Christensen, W. K.: The Albian to Maastrichtian of southern Sweden and
Bornholm, Denmark: a review, Cretaceous Res., 5, 313–327, 1984.
Christensen, W. K.: Paleobiogeography and migration in the Late Cretaceous
belemnite family Belemnitellidae, Acta Palaeontol. Pol., 42,
457–495, 1997.
Clarke, L. J. and Jenkyns, H. C.: New oxygen isotope evidence for long-term
Cretaceous climatic change in the Southern Hemisphere, Geology, 27,
699–702, 1999.
Cochran, J. K., Kallenberg, K., Landman, N. H., Harries, P. J., Weinreb, D.,
Turekian, K. K., Beck, A. J., and Cobban, W. A.: Effect of diagenesis on the
Sr, O, and C isotope composition of late Cretaceous mollusks from the
Western Interior Seaway of North America, Am. J. Sci.,
310, 69–88, https://doi.org/10.2475/02.2010.01, 2010.
Coggon, R. M., Teagle, D. A., Smith-Duque, C. E., Alt, J. C., and Cooper, M.
J.: Reconstructing past seawater Mg∕Ca and Sr/Ca from mid-ocean ridge flank
calcium carbonate veins, Science, 327, 1114–1117, 2010.
Cognie, B., Haure, J., and Barillé, L.: Spatial distribution in a
temperate coastal ecosystem of the wild stock of the farmed oyster
Crassostrea gigas (Thunberg), Aquaculture, 259, 249–259, 2006.
Csiki-Sava, Z., Buffetaut, E., Ősi, A., Pereda-Suberbiola, X., and
Brusatte, S. L.: Island life in the Cretaceous – faunal composition,
biogeography, evolution, and extinction of land-living vertebrates on the
Late Cretaceous European archipelago, Zookeys, 469, 1–161,
https://doi.org/10.3897/zookeys.469.8439, 2015.
Dalbeck, P., England, J., Cusack, M., Lee, M. R., and Fallick, A. E.:
Crystallography and chemistry of the calcium carbonate polymorph switch in
M. edulis shells, Eur. J. Mineral., 18, 601–609,
https://doi.org/10.1127/0935-1221/2006/0018-0601, 2006.
Danielsson, Å., Papush, L., and Rahm, L.: Alterations in
nutrient limitations – scenarios of a changing Baltic Sea, J. Mar.
Syst., 73, 263–283, 2008.
DeConto, R. M., Hay, W. W., Thompson, S. L., and Bergengren, J.: Late
Cretaceous climate and vegetation interactions: cold continental interior
paradox, Special Papers-Geological Society Of America, 332, 391–406, 1999.
De Villiers, S.: Seawater strontium and Sr∕Ca variability in the Atlantic
and Pacific oceans, Earth Planet. Sc. Lett., 171, 623–634,
1999.
Dellinger, M., West, A. J., Paris, G., Adkins, J. F., von Strandmann, P. A.
P., Ullmann, C. V., Eagle, R. A., Freitas, P., Bagard, M.-L., and Ries, J.
B.: The Li isotope composition of marine biogenic carbonates: Patterns and
Mechanisms, Geochim. Cosmochim. Ac., 236, 315–335, 2018.
de Winter, N. J. and Claeys, P.: Micro X-ray fluorescence (µXRF) line
scanning on Cretaceous rudist bivalves: A new method for reproducible trace
element profiles in bivalve calcite, edited by: Petrizzo, M. R.,
Sedimentology, 64, 231–251, https://doi.org/10.1111/sed.12299, 2016.
de Winter, N. J., Sinnesael, M., Makarona, C., Vansteenberge, S., and Claeys,
P.: Trace element analyses of carbonates using portable and micro-X-ray
fluorescence: performance and optimization of measurement parameters and
strategies, J. Anal. Atom. Spectr., 32, 1211–1223,
2017b.
de Winter, N. J., Goderis, S., Dehairs, F., Jagt, J. W., Fraaije, R. H., Van
Malderen, S. J., Vanhaecke, F., and Claeys, P.: Tropical seasonality in the
late Campanian (late Cretaceous): Comparison between multiproxy records from
three bivalve taxa from Oman, Palaeogeogr. Palaeocl., 485, 740–760, 2017a.
de Winter, N. J., Vellekoop, J., Vorsselmans, R., Golreihan, A., Soete, J., Petersen, S. V., Meyer, K. W., Casadio, S., Speijer, R. P., and Claeys, P.: An assessment of latest Cretaceous Pycnodonte vesicularis (Lamarck, 1806) shells as records for palaeoseasonality: a multi-proxy investigation, Clim. Past, 14, 725–749, https://doi.org/10.5194/cp-14-725-2018, 2018.
de Winter, N. J., Goderis, S., Malderen, S. J. M. V., Sinnesael, M.,
Vansteenberge, S., Snoeck, C., Belza, J., Vanhaecke, F., and Claeys, P.:
Subdaily-Scale Chemical Variability in a Torreites Sanchezi Rudist Shell:
Implications for Rudist Paleobiology and the Cretaceous Day-Night Cycle,
Paleoceanogr. Paleocl., 35, PA003723,
https://doi.org/10.1029/2019PA003723, 2020a.
de Winter, N. J., Vellekoop, J., Clark, A. J., Stassen, P., Speijer, R. P.,
and Claeys, P.: The giant marine gastropod Campanile giganteum (Lamarck,
1804) as a high-resolution archive of seasonality in the Eocene greenhouse
world, Geochem. Geophy., Geosy., 21, GC008794,
https://doi.org/10.1029/2019GC008794, 2020b.
de Winter, N. J., Ullmann, C. V., Sorensen, A. M., Thibault, N., Goderis, S., Van Malderen, S. J. M., Snoeck, C., Goolaerts, S., Vanhaecke, F., and Claeys, P.: Supplement to: Shell chemistry of the Boreal Campanian bivalve Rastellum diluvianum (Linnaeus, 1767) reveals temperature seasonality, growth rates and life cycle of an extinct Cretaceous oyster, Zenodo, https://doi.org/10.5281/zenodo.2581304, 2020c.
Donnadieu, Y., Pucéat, E., Moiroud, M., Guillocheau, F., and Deconinck,
J.-F.: A better-ventilated ocean triggered by Late Cretaceous changes in
continental configuration, Nat. Commun., 7, 10316,
https://doi.org/10.1038/ncomms10316, 2016.
El Meknassi, S., Dera, G., Cardone, T., De Rafélis, M., Brahmi, C., and
Chavagnac, V.: Sr isotope ratios of modern carbonate shells: Good and bad
news for chemostratigraphy, Geology, 46, 1003–1006, 2018.
Fan, C., Koeniger, P., Wang, H., and Frechen, M.: Ligamental increments of
the mid-Holocene Pacific oyster Crassostrea gigas are reliable independent
proxies for seasonality in the western Bohai Sea, China, Palaeogeogr.
Palaeocl., 299, 437–448, 2011.
Freitas, P. S., Clarke, L. J., Kennedy, H. A., and Richardson, C. A.: Inter- and intra-specimen variability masks reliable temperature control on shell Mg∕Ca ratios in laboratory- and field-cultured Mytilus edulis and Pecten maximus (bivalvia), Biogeosciences, 5, 1245–1258, https://doi.org/10.5194/bg-5-1245-2008, 2008.
Friedrich, O., Herrle, J. O., and Hemleben, C.: Climatic changes in the late
Campanian – early Maastrichtian: Micropaleontological and stable isotopic
evidence from an epicontinental sea, J. Foramin. Res.,
35, 228–247, 2005.
Friedrich, O., Herrle, J. O., Wilson, P. A., Cooper, M. J., Erbacher, J., and
Hemleben, C.: Early Maastrichtian carbon cycle perturbation and cooling
event: Implications from the South Atlantic Ocean, Paleoceanography, 24,
PA2211, https://doi.org/10.1029/2008PA001654, 2009.
Friedrich, O., Norris, R. D., and Erbacher, J.: Evolution of middle to Late
Cretaceous oceans—a 55 my record of Earth's temperature and carbon cycle,
Geology, 40, 107–110, 2012.
Füllenbach, C. S., Schöne, B. R., and Mertz-Kraus, R.:
Strontium/lithium ratio in aragonitic shells of Cerastoderma edule
(Bivalvia) – A new potential temperature proxy for brackish environments,
Chem. Geol., 417, 341–355, 2015.
Galtsoff, P. S.: The American Oyster: US Fish and Wildlife Service, Fish.
Bull., 64, 480, 1964.
Gillikin, D. P., Lorrain, A., Navez, J., Taylor, J. W., André, L.,
Keppens, E., Baeyens, W., and Dehairs, F.: Strong biological controls on
Sr∕Ca ratios in aragonitic marine bivalve shells, Geochem. Geophy.
Geosy., 6, Q05009, https://doi.org/10.1029/2004GC000874, 2005.
Gillikin, D. P., Lorrain, A., Bouillon, S., Willenz, P. and Dehairs, F.:
Stable carbon isotopic composition of Mytilus edulis shells: relation to
metabolism, salinity, δ13C DIC and phytoplankton, Organic
Geochemistry, 37, 1371–1382, 2006.
Gillikin, D. P., Lorrain, A., Meng, L., and Dehairs, F.: A large metabolic
carbon contribution to the δ13C record in marine aragonitic
bivalve shells, Geochim. Cosmochim. Ac., 71, 2936–2946, 2007.
Goodwin, D. H., Flessa, K. W., Schone, B. R., and Dettman, D. L.: Cross-calibration of daily growth increments, stable isotope variation, and temperature in the Gulf of California bivalve mollusk Chione cortezi: implications for paleoenvironmental analysis, Palaios, 16, 387–398, 2001.
Grossman, E. L. and Ku, T.-L.: Oxygen and carbon isotope fractionation in biogenic aragonite: temperature effects, Chemical Geology: Isotope Geoscience section, 59, 59–74, 1986.
Hart, D. R. and Chute, A. S.: Verification of Atlantic sea scallop
(Placopecten magellanicus) shell growth rings by tracking cohorts in fishery
closed areas, Can. J. Fish. Aquat. Sci., 66,
751–758, 2009.
Hay, W. W. and Floegel, S.: New thoughts about the Cretaceous climate and
oceans, Earth-Sci. Rev., 115, 262–272, 2012.
Högdahl, K., Andersson, U. B., and Eklund, O.: The Transscandinavian
Igneous Belt (TIB) in Sweden: a review of its character and evolution,
Geol. Surv. Finland Espoo, 37, 1–25, 2004.
Huber, B. T., Norris, R. D., and MacLeod, K. G.: Deep-sea paleotemperature
record of extreme warmth during the Cretaceous, Geology, 30, 123–126,
2002.
Huck, S., Heimhofer, U., Rameil, N., Bodin, S., and Immenhauser, A.:
Strontium and carbon-isotope chronostratigraphy of Barremian–Aptian
shoal-water carbonates: Northern Tethyan platform drowning predates OAE 1a,
Earth Planet. Sc. Lett., 304, 547–558,
https://doi.org/10.1016/j.epsl.2011.02.031, 2011.
Huyghe, D., Lartaud, F., Emmanuel, L., Merle, D., and Renard, M.: Palaeogene
climate evolution in the Paris Basin from oxygen stable isotope (δ18O) compositions of marine molluscs, J. Geol. Soc.,
172, 576–587, 2015.
Huyghe, D., de Rafelis, M., Ropert, M., Mouchi, V., Emmanuel, L., Renard, M.,
and Lartaud, F.: New insights into oyster high-resolution hinge growth
patterns, Mar. Biol., 166, 1–17, https://doi.org/10.1007/s00227-019-3496-2, 2019.
Immenhauser, A., Nägler, T. F., Steuber, T., and Hippler, D.: A critical
assessment of mollusk 18O∕16O, Mg∕Ca, and 44Ca∕40Ca ratios as proxies
for Cretaceous seawater temperature seasonality, Palaeogeogr.
Palaeocl., 215, 221–237, 2005.
International Research Institute for Climate and Society: IRI/LDEO Climate Data Library, available at: http://iridl.ldeo.columbia.edu, last access:
6 March 2020.
IPCC: IPCC, 2013: Climate Change 2013: The Physical Science Basis,
Contribution of Working Group I to the Fifth Assessment Report of the
Intergovernmental Panel on Climate Change, Cambridge Univ. Press,
Cambridge, UK, and New York, 1535 pp., 2013.
Ivany, L. C.: Reconstructing paleoseasonality from accretionary skeletal
carbonates – challenges and opportunities, Paleontological Society
Papers, 18, 133–166, 2012.
Ivany, L. C. and Runnegar, B.: Early Permian seasonality from bivalve
δ18O and implications for the oxygen isotopic composition of
seawater, Geology, 38, 1027–1030, 2010.
Jablonski, D., Huang, S., Roy, K., and Valentine, J. W.: Shaping the
latitudinal diversity gradient: new perspectives from a synthesis of
paleobiology and biogeography, Am. Nat., 189, 1–12, 2017.
Jarvis, I., Mabrouk, A., Moody, R. T., and de Cabrera, S.: Late Cretaceous
(Campanian) carbon isotope events, sea-level change and correlation of the
Tethyan and Boreal realms, Palaeogeogr. Palaeocl., 188, 215–248, 2002.
Jenkyns, H. C., Gale, A. S., and Corfield, R. M.: Carbon-and oxygen-isotope
stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic
significance, Geol. Mag., 131, 1–34, 1994.
Jenkyns, H. C., Forster, A., Schouten, S., and Damsté, J. S. S.: High
temperatures in the late Cretaceous Arctic Ocean, Nature, 432, 888–892,
2004.
Jones, D. S.: Sclerochronology: reading the record of the molluscan shell:
annual growth increments in the shells of bivalve molluscs record marine
climatic changes and reveal surprising longevity, Am. Sci., 71,
384–391, 1983.
Judd, E. J., Wilkinson, B. H., and Ivany, L. C.: The life and time of clams:
Derivation of intra-annual growth rates from high-resolution oxygen isotope
profiles, Palaeogeogr. Palaeocl., 490, 70–83,
2018.
Kawaguchi, T. and Watabe, N.: The organic matrices of the shell of the
American oyster Crassostrea virginica Gmelin, J. Exp. Mar.
Biol. Ecol., 170, 11–28, https://doi.org/10.1016/0022-0981(93)90126-9, 1993.
Kim, S.-T. and O'Neil, J. R.: Equilibrium and nonequilibrium oxygen isotope
effects in synthetic carbonates, Geochim. Cosmochim. Ac., 61,
3461–3475, 1997.
Klein, R. T., Lohmann, K. C., and Thayer, C. W.: Bivalve skeletons record
sea-surface temperature and δ18O via Mg∕Ca and 18O∕16O ratios,
Geology, 24, 415–418, 1996a.
Klein, R. T., Lohmann, K. C., and Thayer, C. W.: SrCa and 13C12C ratios in
skeletal calcite of Mytilus trossulus: Covariation with metabolic rate,
salinity, and carbon isotopic composition of seawater, Geochim.
Cosmochim. Ac., 60, 4207–4221, https://doi.org/10.1016/S0016-7037(96)00232-3,
1996b.
Kominz, M. A., Browning, J. V., Miller, K. G., Sugarman, P. J., Mizintseva,
S., and Scotese, C. R.: Late Cretaceous to Miocene sea-level estimates from
the New Jersey and Delaware coastal plain coreholes: an error analysis,
Basin Res., 20, 211–226, 2008.
Krantz, D. E., Williams, D. F., and Jones, D. S.: Ecological and
paleoenvironmental information using stable isotope profiles from living and
fossil molluscs, Palaeogeogr. Palaeocl., 58,
249–266, https://doi.org/10.1016/0031-0182(87)90064-2, 1987.
Kuznetsov, A. B., Semikhatov, M. A., and Gorokhov, I. M.: The Sr isotope
composition of the world ocean, marginal and inland seas: Implications for
the Sr isotope stratigraphy, Stratigr. Geol. Correl., 20, 501–515,
https://doi.org/10.1134/S0869593812060044, 2012.
Lartaud, F., Emmanuel, L., De Rafélis, M., Ropert, M., Labourdette, N.,
Richardson, C. A., and Renard, M.: A latitudinal gradient of seasonal
temperature variation recorded in oyster shells from the coastal waters of
France and The Netherlands, Facies, 56, 13–25, 2010.
Lear, C. H., Elderfield, H., and Wilson, P. A.: A Cenozoic seawater Sr/Ca
record from benthic foraminiferal calcite and its application in determining
global weathering fluxes, Earth Planet. Sc. Lett., 208,
69–84, https://doi.org/10.1016/S0012-821X(02)01156-1, 2003.
Li, Y., Qin, J. G., Abbott, C. A., Li, X., and Benkendorff, K.: Synergistic
impacts of heat shock and spawning on the physiology and immune health of
Crassostrea gigas: an explanation for summer mortality in Pacific oysters,
Am. J. Physiol.-Reg. I., 293, R2353–R2362, 2007.
Locarnini, R. A., Mishonov, A. V., Antonov, J. I., Boyer, T. P., Garcia, H.
E., Baranova, O. K., Zweng, M. M., Paver, C. R., Reagan, J. R., Johnson, D.
R., Hamilton, M., and Seidov, D.: World ocean atlas 2013. Volume 1,
Temperature, U.S. Department of Commerce, National Oceanic and Atmospheric
Administration, National Environmental Satellite, Data and Information
Service, https://doi.org/10.7289/v55x26vd, 2013.
Lorrain, A., Paulet, Y.-M., Chauvaud, L., Dunbar, R., Mucciarone, D., and
Fontugne, M.: δ13C variation in scallop shells: increasing
metabolic carbon contribution with body size?, Geochim. Cosmochim.
Ac., 68, 3509–3519, 2004.
Lorrain, A., Gillikin, D. P., Paulet, Y.-M., Chauvaud, L., Le Mercier, A.,
Navez, J., and André, L.: Strong kinetic effects on Sr∕Ca ratios in the
calcitic bivalve Pecten maximus, Geology, 33, 965–968, 2005.
Lowenstam, H. A. and Epstein, S.: Paleotemperatures of the post-Aptian
Cretaceous as determined by the oxygen isotope method, J.
Geol., 62, 207–248, 1954.
MacDonald, B. A. and Thompson, R. J.: Influence of temperature and food
availability on the ecological energetics of the giant scallop Placopecten
magellanicus, I. Growth rates of shell and somatic tissue, Marine ecology
progress series, Oldendorf, 25, 279–294, 1985.
Marchais, V., Richard, J., Jolivet, A., Flye-Sainte-Marie, J., Thébault,
J., Jean, F., Richard, P., Paulet, Y.-M., Clavier, J., and Chauvaud, L.:
Coupling experimental and field-based approaches to decipher carbon sources
in the shell of the great scallop, Pecten maximus (L.), Geochim. .
Cosmochim. Ac., 168, 58–69, https://doi.org/10.1016/j.gca.2015.07.010, 2015.
McArthur, J. M., Howarth, R. J., and Bailey, T. R.: Strontium Isotope
Stratigraphy: LOWESS Version 3: Best Fit to the Marine Sr-Isotope Curve for
0–509 Ma and Accompanying Look-up Table for Deriving Numerical Age,
J. Geol., 109, 155–170, https://doi.org/10.1086/319243, 2001.
McArthur, J. M., Steuber, T., Page, K. N., and Landman, N. H.: Sr-isotope
stratigraphy: assigning time in the Campanian, Pliensbachian, Toarcian, and
Valanginian, J. Geol., 124, 569–586, 2016.
McConnaughey, T. A.: Sub-equilibrium oxygen-18 and carbon-13 levels in
biological carbonates: carbonate and kinetic models, Coral Reefs, 22,
316–327, 2003.
McConnaughey, T. A. and Gillikin, D. P.: Carbon isotopes in mollusk shell
carbonates, Geo-Mar. Lett., 28 287–299,
https://doi.org/10.1007/s00367-008-0116-4, 2008.
McConnaughey, T. A., Burdett, J., Whelan, J. F., and Paull, C. K.: Carbon
isotopes in biological carbonates: respiration and photosynthesis,
Geochim. Cosmochim. Ac., 61, 611–622, 1997.
Miller, K. G., Wright, J. D., and Browning, J. V.: Visions of ice sheets in a
greenhouse world, Mar. Geol., 217, 215–231,
https://doi.org/10.1016/j.margeo.2005.02.007, 2005.
Montgomery, P., Hailwood, E. A., Gale, A. S., and Burnett, J. A.: The
magnetostratigraphy of Coniacian-Late Campanian chalk sequences in southern
England, Earth Planet. Sc. Lett., 156, 209–224,
https://doi.org/10.1016/S0012-821X(98)00008-9, 1998.
Mook, W. G.: Paleotemperatures and chlorinities from stable carbon and
oxygen isotopes in shell carbonate, Palaeogeogr. Palaeocl., 9, 245–263, https://doi.org/10.1016/0031-0182(71)90002-2, 1971.
Mouchi, V., De Rafélis, M., Lartaud, F., Fialin, M., and Verrecchia, E.:
Chemical labelling of oyster shells used for time-calibrated high-resolution
Mg∕Ca ratios: a tool for estimation of past seasonal temperature variations,
Palaeogeogr. Palaeocl., 373, 66–74, 2013.
NOAA Earth System Research Laboratory: NOAA Optimum Interpolation (IO) Sea
Surface Temperature (SST), available at:
http://www.esrl.noaa.gov/psd/data/gridded/data.noaa.oisst.v2.html, last access: 21 January 2019.
O'Brien, C. L., Robinson, S. A., Pancost, R. D., Sinninghe Damsté, J.
S., Schouten, S., Lunt, D. J., Alsenz, H., Bornemann, A., Bottini, C.,
Brassell, S. C., Farnsworth, A., Forster, A., Huber, B. T., Inglis, G. N.,
Jenkyns, H. C., Linnert, C., Littler, K., Markwick, P., McAnena, A.,
Mutterlose, J., Naafs, B. D. A., Püttmann, W., Sluijs, A., van Helmond,
N. A. G. M., Vellekoop, J., Wagner, T., and Wrobel, N. E.: Cretaceous
sea-surface temperature evolution: Constraints from TEX 86 and planktonic
foraminiferal oxygen isotopes, Earth-Sci. Rev., 172, 224–247,
https://doi.org/10.1016/j.earscirev.2017.07.012, 2017.
Ogg, J. G., Ogg, G., and Gradstein, F. M.: A concise geologic time scale:
2016, Elsevier, 1–231, 2016.
Palmer, R. E. and Carriker, M. R.: Effects of cultural conditions on
morphology of the shell of the oyster Crassostrea virginica, in: Proceedings
of the National Shellfisheries Association, Vol. 69, 58–72, 1979.
Pearson, P. N., Ditchfield, P. W., Singano, J., Harcourt-Brown, K. G.,
Nicholas, C. J., Olsson, R. K., Shackleton, N. J., and Hall, M. A.: Warm
tropical sea surface temperatures in the Late Cretaceous and Eocene epochs,
Nature, 413, 481–487, 2001.
Perdiou, A., Thibault, N., Anderskouv, K., Van Buchem, F., Buijs, G. J. A.,
and Bjerrum, C. J.: Orbital calibration of the late Campanian carbon isotope
event in the North Sea, J. Geol. Soc., 173, 504–517,
2016.
Prandle, D. and Lane, A.: The annual temperature cycle in shelf seas,
Cont. Shelf Res., 15, 681–704,
https://doi.org/10.1016/0278-4343(94)E0029-L, 1995.
Rausch, S., Böhm, F., Bach, W., Klügel, A., and Eisenhauer, A.:
Calcium carbonate veins in ocean crust record a threefold increase of
seawater Mg/Ca in the past 30 million years, Earth Planet. Sc.
Lett., 362, 215–224, 2013.
Rayner, N. A., Parker, D. E., Horton, E. B., Folland, C. K., Alexander, L.
V., Rowell, D. P., Kent, E. C., and Kaplan, A.: Global analyses of sea
surface temperature, sea ice, and night marine air temperature since the
late nineteenth century, J. Geophys. Res.-Atmos.,
108, 1–22, https://doi.org/10.1029/2002JD002670, 2003.
R Core Team: R: A language and environment for statistical computing, R foundation for statistical computing, Vienna, Austria, 2008.
Reid, R. E. H.: The Chalk Sea, The Irish Naturalists' Journal, 17,
357–375, 1973.
Richardson, C. A., Peharda, M., Kennedy, H., Kennedy, P., and Onofri, V.:
Age, growth rate and season of recruitment of Pinna nobilis (L) in the
Croatian Adriatic determined from Mg: Ca and Sr: Ca shell profiles, J. Exp. Mar. Biol. Ecol., 299, 1–16, 2004.
Roy, K., Jablonski, D., and Martien, K. K.: Invariant size–frequency
distributions along a latitudinal gradient in marine bivalves, P. Natl. Acad. Sci. USA, 97,
13150–13155, https://doi.org/10.1073/pnas.97.24.13150, 2000.
Rucker, J. B. and Valentine, J. W.: Salinity Response of Trace Element
Concentration in Crassostrea virginica, Nature, 190, 1099–1100,
https://doi.org/10.1038/1901099a0, 1961.
Sano, Y., Kobayashi, S., Shirai, K., Takahata, N., Matsumoto, K., Watanabe,
T., Sowa, K., and Iwai, K.: Past daily light cycle recorded in the
strontium/calcium ratios of giant clam shells, Nat. Commun., 3, 1–6,
https://doi.org/10.1038/ncomms1763, 2012.
Schöne, B. R. and Gillikin, D. P.: Unraveling environmental histories
from skeletal diaries – Advances in sclerochronology, Palaeogeogr.
Palaeocl., 373, 1–5,
https://doi.org/10.1016/j.palaeo.2012.11.026, 2013.
Schöne, B. R., Houk, S. D., Freyre Castro, A. D., Fiebig, J., Oschmann,
W., KröNcke, I., Dreyer, W., and Gosselck, F.: Daily growth rates in
shells of Arctica islandica: assessing sub-seasonal environmental controls
on a long-lived bivalve mollusk, Palaios, 20, 78–92, 2005.
Schöne, B. R., Zhang, Z., Jacob, D., Gillikin, D. P., Tütken, T.,
Garbe-Schönberg, D., McConnaughey, T., and Soldati, A.: Effect of organic
matrices on the determination of the trace element chemistry (Mg, Sr, Mg∕Ca,
Sr∕Ca) of aragonitic bivalve shells (Arctica islandica) – Comparison of
ICP-OES and LA-ICP-MS data, Geochem. J., 44, 23–37, 2010.
Schöne, B. R., Zhang, Z., Radermacher, P., Thébault, J., Jacob, D.
E., Nunn, E. V., and Maurer, A.-F.: Sr/Ca and Mg/Ca ratios of ontogenetically
old, long-lived bivalve shells (Arctica islandica) and their function as
paleotemperature proxies, Palaeogeogr. Palaeocl.,
302, 52–64, 2011.
Schöne, B. R., Radermacher, P., Zhang, Z., and Jacob, D. E.: Crystal
fabrics and element impurities (Sr∕Ca, Mg∕Ca, and Ba∕Ca) in shells of
Arctica islandica – Implications for paleoclimate reconstructions,
Palaeogeogr. Palaeocl., 373, 50–59, 2013.
Scotese, C.: A New Global Temperature Curve For The Phanerozoic, GSA Annual Meeting Denver, Colorado, Abstracts with Programs, Vol. 48, No. 7, 2016.
Shackleton, N. J.: Paleogene stable isotope events, Palaeogeogr.
Palaeocl., 57, 91–102, 1986.
Snoeck, C., Lee-Thorp, J., Schulting, R., Jong, J., Debouge, W., and
Mattielli, N.: Calcined bone provides a reliable substrate for strontium
isotope ratios as shown by an enrichment experiment, Rapid Commun.
Mass Sp., 29, 107–114, 2015.
Sørensen, A. M., Surlyk, F., and Jagt, J. W. M.: Adaptive morphologies and
guild structure in a high-diversity bivalve fauna from an early Campanian
rocky shore, Ivö Klack (Sweden), Cretaceous Res., 33, 21–41,
https://doi.org/10.1016/j.cretres.2011.07.004, 2012.
Sørensen, A. M., Ullmann, C. V., Thibault, N., and Korte, C.: Geochemical
signatures of the early Campanian belemnite Belemnellocamax mammillatus from
the Kristianstad Basin in Scania, Sweden, Palaeogeogr.
Palaeocl., 433, 191–200, 2015.
Stanley, S. M. and Hardie, L. A.: Secular oscillations in the carbonate
mineralogy of reef-building and sediment-producing organisms driven by
tectonically forced shifts in seawater chemistry, Palaeogeogr.
Palaeocl., 144, 3–19, 1998.
Stenzel, H. B.: Aragonite and calcite as constituents of adult oyster
shells, Science, 142, 232–233, 1963.
Steuber, T.: Isotopic and chemical intra-shell variations in low-Mg calcite
of rudist bivalves (Mollusca-Hippuritacea): disequilibrium fractionations
and late Cretaceous seasonality, Int. J. Earth Sci.,
88, 551–570, 1999.
Steuber, T., Rauch, M., Masse, J.-P., Graaf, J., and Malkoč, M.:
Low-latitude seasonality of Cretaceous temperatures in warm and cold
episodes, Nature, 437, 1341–1344, 2005.
Strahl, J., Philipp, E., Brey, T., Broeg, K., and Abele, D.: Physiological
aging in the Icelandic population of the ocean quahog Arctica islandica,
Aquat. Biol., 1, 77–83, 2007.
Surge, D. and Lohmann, K. C.: Evaluating Mg∕Ca ratios as a temperature proxy
in the estuarine oyster, Crassostrea virginica, J. Geophys.
Res.-Biogeo., 113, 1–9, https://doi.org/10.1029/2007JG000623, 2008.
Surge, D., Lohmann, K. C., and Dettman, D. L.: Controls on isotopic chemistry
of the American oyster, Crassostrea virginica: implications for growth
patterns, Palaeogeogr. Palaeocl., 172,
283–296, 2001.
Surge, D. M., Lohmann, K. C., and Goodfriend, G. A.: Reconstructing estuarine
conditions: oyster shells as recorders of environmental change, Southwest
Florida, Estuarine, Coast. Shelf Sci., 57, 737–756,
https://doi.org/10.1016/S0272-7714(02)00370-0, 2003.
Surlyk, F. and Christensen, W. K.: Epifaunal zonation on an Upper Cretaceous
rocky coast, Geology, 2, 529–534, 1974.
Surlyk, F. and Sørensen, A. M.: An early Campanian rocky shore at Ivö
Klack, southern Sweden, Cretaceous Res., 31, 567–576, 2010.
Tagliavento, M., John, C. M., and Stemmerik, L.: Tropical temperature in the
Maastrichtian Danish Basin: Data from coccolith Δ47 and δ18O, Geology, 47, 1074–1078, 2019.
Thibault, N., Husson, D., Harlou, R., Gardin, S., Galbrun, B., Huret, E., and
Minoletti, F.: Astronomical calibration of upper Campanian–Maastrichtian
carbon isotope events and calcareous plankton biostratigraphy in the Indian
Ocean (ODP Hole 762C): Implication for the age of the
Campanian–Maastrichtian boundary, Palaeogeogr. Palaeocl., 337/338, 52–71, https://doi.org/10.1016/j.palaeo.2012.03.027, 2012.
Thibault, N., Harlou, R., Schovsbo, N. H., Stemmerik, L., and Surlyk, F.: Late Cretaceous (late Campanian–Maastrichtian) sea-surface temperature record of the Boreal Chalk Sea, Clim. Past, 12, 429–438, https://doi.org/10.5194/cp-12-429-2016, 2016.
Uchikawa, J. and Zeebe, R. E.: The effect of carbonic anhydrase on the
kinetics and equilibrium of the oxygen isotope exchange in the CO2–H2O
system: Implications for δ18O vital effects in biogenic carbonates,
Geochim. Cosmochim. Ac., 95, 15–34, 2012.
Ullmann, C. V. and Korte, C.: Diagenetic alteration in low-Mg calcite from
macrofossils: a review, Geol. Quart., 59, 3–20, 2015.
Ullmann, C. V., Wiechert, U., and Korte, C.: Oxygen isotope fluctuations in a
modern North Sea oyster (Crassostrea gigas) compared with annual variations
in seawater temperature: Implications for palaeoclimate studies, Chem.
Geol., 277, 160–166, 2010.
Ullmann, C. V., Böhm, F., Rickaby, R. E., Wiechert, U., and Korte, C.:
The Giant Pacific Oyster (Crassostrea gigas) as a modern analog for fossil
ostreoids: isotopic (Ca, O, C) and elemental (Mg∕Ca, Sr∕Ca, Mn∕Ca) proxies,
Geochem. Geophy. Geosy., 14, 4109–4120, 2013.
Upchurch Jr, G. R., Kiehl, J., Shields, C., Scherer, J., and Scotese, C.:
Latitudinal temperature gradients and high-latitude temperatures during the
latest Cretaceous: Congruence of geologic data and climate models, Geology,
43, 683–686, 2015.
van Hinsbergen, D. J., de Groot, L. V., van Schaik, S. J., Spakman, W.,
Bijl, P. K., Sluijs, A., Langereis, C. G., and Brinkhuis, H.: A paleolatitude
calculator for paleoclimate studies, PloS one, 10, e0126946, https://doi.org/10.1371/journal.pone.0126946, 2015.
Vansteenberge, S., de Winter, N. J., Sinnesael, M., Xueqin, Z., Verheyden,
S., and Claeys, P.: Benchtop μXRF as a tool for speleothem trace
elemental analysis: Validation, limitations and application on an Eemian to
early Weichselian (125–97 ka) stalagmite from Belgium, Palaeogeogr.
Palaeocl., 538, 109460,
https://doi.org/10.1016/j.palaeo.2019.109460, 2020.
Veizer, J.: Chemical diagenesis of carbonates: theory and application, Stable isotopes in sedimentary geology, 10, 3–100, 1983.
Veizer, J. and Prokoph, A.: Temperatures and oxygen isotopic composition of
Phanerozoic oceans, Earth-Sci. Rev., 146, 92–104, 2015.
Voigt, S. and Schönfeld, J.: Cyclostratigraphy of the reference section
for the Cretaceous white chalk of northern Germany,
Lägerdorf–Kronsmoor: A late Campanian–early Maastrichtian orbital time
scale, Palaeogeogr. Palaeocl., 287, 67–80,
https://doi.org/10.1016/j.palaeo.2010.01.017, 2010.
Voigt, S., Friedrich, O., Norris, R. D., and Schönfeld, J.:
Campanian–Maastrichtian carbon isotope stratigraphy: shelf-ocean
correlation between the European shelf sea and the tropical Pacific Ocean,
Newsl. Stratigr., 44, 57–72, 2010.
von Bertalanffy, L.: Quantitative laws in metabolism and growth, Q. Rev. Biol., 32, 217–231, 1957.
Waniek, J. J.: The role of physical forcing in initiation of spring blooms
in the northeast Atlantic, J. Mar. Syst., 39, 57–82,
2003.
Warter, V., Erez, J., and Müller, W.: Environmental and physiological
controls on daily trace element incorporation in Tridacna crocea from
combined laboratory culturing and ultra-high resolution LA-ICP-MS analysis,
Palaeogeogr. Palaeocl., 496, 32–47,
https://doi.org/10.1016/j.palaeo.2017.12.038, 2018.
Watanabe, T., Suzuki, A., Kawahata, H., Kan, H., and Ogawa, S.: A 60-year
isotopic record from a mid-Holocene fossil giant clam (Tridacna gigas) in
the Ryukyu Islands: physiological and paleoclimatic implications,
Palaeogeogr. Palaeocl., 212, 343–354,
2004.
Weiner, S. and Dove, P. M.: An overview of biomineralization processes and
the problem of the vital effect, Rev. Mineral. Geochem.,
54, 1–29, 2003.
Weis, D., Kieffer, B., Maerschalk, C., Barling, J., Jong, J. de, Williams,
G. A., Hanano, D., Pretorius, W., Mattielli, N., Scoates, J. S., Goolaerts,
A., Friedman, R. M., and Mahoney, J. B.: High-precision isotopic
characterization of USGS reference materials by TIMS and MC-ICP-MS,
Geochem. Geophy. Geosy., 7, Q08006,
https://doi.org/10.1029/2006GC001283, 2006.
Wendler, I.: A critical evaluation of carbon isotope stratigraphy and
biostratigraphic implications for Late Cretaceous global correlation,
Earth-Sci. Rev., 126, 116–146, https://doi.org/10.1016/j.earscirev.2013.08.003,
2013.
Yang, D., Huang, Y., Guo, W., Huang, Q., Ren, Y., and Wang, C.: Late
Santonian-early Campanian lake-level fluctuations in the Songliao Basin, NE
China and their relationship to coeval eustatic changes, Cretaceous
Res., 92, 138–149, https://doi.org/10.1016/j.cretres.2018.07.008, 2018.
Yoshimura, T., Tanimizu, M., Inoue, M., Suzuki, A., Iwasaki, N., and
Kawahata, H.: Mg isotope fractionation in biogenic carbonates of deep-sea
coral, benthic foraminifera, and hermatypic coral, Anal. Bioanal. Chem.,
401, 2755, https://doi.org/10.1007/s00216-011-5264-0, 2011.
Zimmt, J. B., Lockwood, R., Andrus, C. F. T., and Herbert, G. S.:
Sclerochronological basis for growth band counting: A reliable technique for
life-span determination of Crassostrea virginica from the mid-Atlantic
United States, Palaeogeogr. Palaeocl., 516,
54–63, 2018.
Short summary
In this study, we present a detailed investigation of the chemical composition of 12 specimens of very well preserved, 78-million-year-old oyster shells from southern Sweden. The chemical data show how the oysters grew, the environment in which they lived and how old they became and also provide valuable information about which chemical measurements we can use to learn more about ancient climate and environment from such shells. In turn, this can help improve climate reconstructions and models.
In this study, we present a detailed investigation of the chemical composition of 12 specimens...
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