@article{KallmeyerGreweGlombitzaetal.2015,
  author    = {Kallmeyer, Jens and Grewe, Sina and Glombitza, Clemens and Kitte, J. Axel},
  title     = {Microbial abundance in lacustrine sediments: a case study from Lake Van, Turkey},
  series = {International journal of earth sciences},
  volume    = {104},
  journal   = {International journal of earth sciences},
  number    = {6},
  publisher = {Springer},
  address   = {New York},
  issn      = {1437-3254},
  doi       = {10.1007/s00531-015-1219-6},
  pages     = {1667 -- 1677},
  year      = {2015},
  abstract  = {The ICDP "PaleoVan" drilling campaign at Lake Van, Turkey, provided a long (> 100 m) record of lacustrine subsurface sedimentary microbial cell abundance. After the ICDP campaign at Potrok Aike, Argentina, this is only the second time deep lacustrine cell counts have been documented. Two sites were cored and revealed a strikingly similar cell distribution despite differences in organic matter content and microbial activity. Although shifted towards higher values, cell counts from Lake Potrok Aike, Argentina, reveal very similar distribution patterns with depth. The lacustrine cell count data are significantly different from published marine records; the most probable cause is differences in sedimentary organic matter composition with marine sediments containing a higher fraction of labile organic matter. Previous studies showed that microbial activity and abundance increase centimetres to metres around geologic interfaces. The finely laminated Lake Van sediment allowed studying this phenomenon on the microscale. We sampled at the scale of individual laminae, and in some depth intervals, we found large differences in microbial abundance between the different laminae. This small-scale heterogeneity is normally overlooked due to much larger sampling intervals that integrate over several centimetres. However, not all laminated intervals exhibit such large differences in microbial abundance, and some non-laminated horizons show large variability on the millimetre scale as well. The reasons for such contrasting observations remain elusive, but indicate that heterogeneity of microbial abundance in subsurface sediments has not been taken into account sufficiently. These findings have implications not just for microbiological studies but for geochemistry as well, as the large differences in microbial abundance clearly show that there are distinct microhabitats that deviate considerably from the surrounding layers.},
  language  = {en}
}
@misc{KallmeyerGreweGlombitzaetal.2015,
  author    = {Kallmeyer, Jens and Grewe, Sina and Glombitza, Clemens and Kitte, J. Axel},
  title     = {Microbial abundance in lacustrine sediments},
  series = {Postprints der Universit{\"a}t Potsdam Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Postprints der Universit{\"a}t Potsdam Mathematisch-Naturwissenschaftliche Reihe},
  number    = {723},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-42982},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-429828},
  pages     = {1667 -- 1677},
  year      = {2015},
  abstract  = {The ICDP "PaleoVan" drilling campaign at Lake Van, Turkey, provided a long (> 100 m) record of lacustrine subsurface sedimentary microbial cell abundance. After the ICDP campaign at Potrok Aike, Argentina, this is only the second time deep lacustrine cell counts have been documented. Two sites were cored and revealed a strikingly similar cell distribution despite differences in organic matter content and microbial activity. Although shifted towards higher values, cell counts from Lake Potrok Aike, Argentina, reveal very similar distribution patterns with depth. The lacustrine cell count data are significantly different from published marine records; the most probable cause is differences in sedimentary organic matter composition with marine sediments containing a higher fraction of labile organic matter. Previous studies showed that microbial activity and abundance increase centimetres to metres around geologic interfaces. The finely laminated Lake Van sediment allowed studying this phenomenon on the microscale. We sampled at the scale of individual laminae, and in some depth intervals, we found large differences in microbial abundance between the different laminae. This small-scale heterogeneity is normally overlooked due to much larger sampling intervals that integrate over several centimetres. However, not all laminated intervals exhibit such large differences in microbial abundance, and some non-laminated horizons show large variability on the millimetre scale as well. The reasons for such contrasting observations remain elusive, but indicate that heterogeneity of microbial abundance in subsurface sediments has not been taken into account sufficiently. These findings have implications not just for microbiological studies but for geochemistry as well, as the large differences in microbial abundance clearly show that there are distinct microhabitats that deviate considerably from the surrounding layers.},
  language  = {en}
}
@phdthesis{Grewe2016,
  author    = {Grewe, Sina},
  title     = {Hydro- and biogeochemical investigations of lake sediments in the Kenyan Rift Valley},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-98342},
  school      = {Universit{\"a}t Potsdam},
  pages     = {110},
  year      = {2016},
  abstract  = {Die Seen im kenianischen Riftsystem bieten die einmalige Gelegenheit eine große Bandbreite an hydrochemischen Umweltbedingungen zu studieren, die von S{\"u}ßwasserseen bis hin zu hochsalinen und alkalinen Seen reichen. Da wenig {\"u}ber die hydro- und biogeochemischen Bedingungen in den darunterliegenden Seesedimenten bekannt ist, war es das Ziel dieser Arbeit, bereits existierende Datens{\"a}tze mit Daten aus der Porenwasser- und Biomarker-Analyse zu erweitern. Zus{\"a}tzlich wurden reduzierte Schwefelkomponenten und Sulfatreduktionsraten in den Sedimenten bestimmt. Mit den neu gewonnenen Daten wurde der anthropogene und mikrobielle Einfluss auf die Seesedimente untersucht sowie der Einfluss der Wasserchemie auf den Abbau und den Erhalt von organischem Material im Sediment. Zu den untersuchten Seen geh{\"o}rten: Logipi, Eight (ein kleiner Kratersee in der Region Kangirinyang), Baringo, Bogoria, Naivasha, Oloiden und Sonachi. Die Biomarker-Zusammensetzungen in den untersuchten Seesedimenten waren {\"a}hnlich; allerdings gab es einige Unterschiede zwischen den salinen Seen und den S{\"u}ßwasserseen. Einer dieser Unterschiede war das Vorkommen eines mit β-Carotin verwandten Molek{\"u}ls, das nur in den salinen Seen gefunden wurde. Dieses Molek{\"u}l stammt wahrscheinlich von Cyanobakterien, Einzellern die in großer Anzahl in salinen Seen vorkommen. In den beiden S{\"u}ßwasserseen wurde Stigmasterol gefunden, ein f{\"u}r S{\"u}ßwasseralgen charakteristisches Sterol. In dieser Studie hat sich gezeigt, dass Bogoria und Sonachi f{\"u}r Umweltrekonstruktionen mit Biomarkern besonders gut geeignet sind, da die Abwesenheit von Sauerstoff an deren Seegr{\"u}nden den Abbau von organischem Material verlangsamt. Andere Seen, wie zum Beispiel Naivasha, sind aufgrund des großen anthropogenen Einflusses weniger gut f{\"u}r solche Rekonstruktionen geeignet. Die Biomarker-Analyse bot jedoch die M{\"o}glichkeit, den menschlichen Einfluss auf den See zu studieren. Desweiteren zeigte diese Studie, dass sich Horizonte mit einem hohen Anteil an elementarem Schwefel als temporale Marker nutzen lassen. Diese Horizonte wurden zu einer Zeit abgelagert, als die Wasserpegel sehr niedrig waren. Der Schwefel wurde von Mikroorganismen abgelagert, die zu anoxygener Photosynthese oder Sulfidoxidation f{\"a}hig sind.},
  language  = {en}
}