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000135226 0247_ $$2doi$$a10.1007/s10933-013-9723-9
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000135226 037__ $$aFZJ-2013-03186
000135226 041__ $$aEnglish
000135226 082__ $$a930
000135226 1001_ $$0P:(DE-HGF)0$$aVuillemin, A.$$b0$$eCorresponding author
000135226 245__ $$aOrigin and significance of diagenetic concretions in sediments of Laguna Potrok Aike, southern Argentina
000135226 260__ $$aDordrecht [u.a.]$$bSpringer Science + Business Media B.V$$c2013
000135226 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1396512759_15498
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000135226 520__ $$aAuthigenic minerals can form in the water column and sediments of lakes, either abiotically or mediated by biological activity. Such minerals have been used as paleosalinity and paleoproductivity indicators and reflect trophic state and early diagenetic conditions. They are also considered potential indicators of past and perhaps ongoing microbial activity within sediments. Authigenic concretions, including vivianite, were described in late glacial sediments of Laguna Potrok Aike, a maar lake in southernmost Argentina. Occurrence of iron phosphate implies specific phosphorus sorption behavior and a reducing environment, with methane present. Because organic matter content in these sediments was generally low during glacial times, there must have been alternative sources of phosphorus and biogenic methane. Identifying these sources can help define past trophic state of the lake and diagenetic processes in the sediments. We used scanning electron microscopy, phosphorus speciation in bulk sediment, pore water analyses, in situ ATP measurements, microbial cell counts, and measurements of methane content and its carbon isotope composition (δ13CCH4) to identify components of and processes in the sediment. The multiple approaches indicated that volcanic materials in the catchment are important suppliers of iron, sulfur and phosphorus. These elements influence primary productivity and play a role in microbial metabolism during early diagenesis. Authigenic processes led to the formation of pyrite framboids and revealed sulfate reduction. Anaerobic oxidation of methane and shifts in pore water ion concentration indicated microbial influence with depth. This study documents the presence of active microbes within the sediments and their relationship to changing environmental conditions. It also illustrates the substantial role played by microbes in the formation of Laguna Potrok Aike concretions. Thus, authigenic minerals can be used as biosignatures in these late Pleistocene maar sediments.
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000135226 7001_ $$0P:(DE-Juel1)VDB47980$$aAriztegui, D.$$b1
000135226 7001_ $$0P:(DE-HGF)0$$aConinck, A. S.$$b2
000135226 7001_ $$0P:(DE-Juel1)129567$$aLücke, A.$$b3$$ufzj
000135226 7001_ $$0P:(DE-Juel1)VDB57755$$aMayr, C.$$b4
000135226 7001_ $$0P:(DE-HGF)0$$aSchubert, C. J.$$b5
000135226 773__ $$0PERI:(DE-600)1478181-5$$a10.1007/s10933-013-9723-9$$n3$$p275-291$$tJournal of paleolimnology$$v50$$x1573-0417$$y2013
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