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<article language="en">
	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>4</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/bg-4-195-2007</doi>
	<article_url>http://www.biogeosciences.net/4/195/2007/</article_url>
	<abstract_html>http://www.biogeosciences.net/4/195/2007/bg-4-195-2007.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/4/195/2007/bg-4-195-2007.pdf</fulltext_pdf>
	<start_page>195</start_page>
	<end_page>203</end_page>
	<publication_date>2007-03-15</publication_date>
	<article_title content_type="html">Manganese content records seasonal upwelling in Lake Tanganyika mussels</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Langlet</name>
			<email>dlanglet@africamuseum.be</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>L. Y. Alleman</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P.-D. Plisnier</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>H. Hughes</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>L. André</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Section de Pétrographie-Minéralogie-Géochimie, Musée Royal de l&apos;Afrique Centrale, Leuvensesteenweg 13, 3080 Tervuren, Belgium</affiliation>
	</affiliations>
	<abstract content_type="html">Biogenic productivity of Lake Tanganyika is highly dependent on seasonal
upwellings of cold, oxygen-depleted, nutrient-rich deep waters. We investigated the shell of freshwater
bivalve &lt;i&gt;Pleiodon spekii&lt;/i&gt; as a geochemical archive of these periodic hydrological changes
tuned by the monsoon regime. The results of a three-year-long limnological
and geochemical survey of the coastal waters performed on the dissolved and
particulate fractions were compared to LA-ICP-MS profiles of Mn in five
aragonitic shells from the same lake location. Three shells present very
similar Mn/Ca profiles dominated by a peak that matched the concomitant
increase of Mn and chlorophyll &lt;i&gt;a&lt;/i&gt; in surface waters during the 2002 upwelling,
while a shell collected during 2003 dry season detect both 2002 and 2003
upwelling events. Larger shells showing an extremely reduced growth display
more than 8 Mn/Ca peaks suggesting at least an 8-year-record of seasonal
changes in water composition. We postulate that Mn/Ca in shells record the
conjunction of an increase of biological activity with supplied of dissolved
Mn and nutriments in coastal waters, resulting in an enhanced assimilation
of biogenic Mn-rich particles. By combining the most recent generation of
laser ablation system and the powerful High Resolution ICP-MS, the spatial
resolution could be improved down to 5 to 10 &amp;micro;m crater size and end up
in a better constrain of the relative variations of the annual Mn peaks.
Such an approach on &lt;i&gt;P. spekii&lt;/i&gt; from Lake Tanganyika has definitively a great
potential to provide recent and past records on primary productivity
associated with the monsoon climate system.</abstract>
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</article>

