@article{StolpmannMollenhauerMorgensternetal.2022,
  author    = {Stolpmann, Lydia and Mollenhauer, Gesine and Morgenstern, Anne and Hammes, Jens S. and Boike, Julia and Overduin, Pier Paul and Grosse, Guido},
  title     = {Origin and pathways of dissolved organic carbon in a small catchment in the Lena River Delta},
  series = {Frontiers in Earth Science},
  volume    = {9},
  journal   = {Frontiers in Earth Science},
  publisher = {Frontiers Media},
  address   = {Lausanne},
  issn      = {2296-6463},
  doi       = {10.3389/feart.2021.759085},
  pages     = {15},
  year      = {2022},
  abstract  = {The Arctic is rich in aquatic systems and experiences rapid warming due to climate change. The accelerated warming causes permafrost thaw and the mobilization of organic carbon. When dissolved organic carbon is mobilized, this DOC can be transported to aquatic systems and degraded in the water bodies and further downstream. Here, we analyze the influence of different landscape components on DOC concentrations and export in a small (6.45 km(2)) stream catchment in the Lena River Delta. The catchment includes lakes and ponds, with the flow path from Pleistocene yedoma deposits across Holocene non-yedoma deposits to the river outlet. In addition to DOC concentrations, we use radiocarbon dating of DOC as well as stable oxygen and hydrogen isotopes (delta O-18 and delta D) to assess the origin of DOC. We find significantly higher DOC concentrations in the Pleistocene yedoma area of the catchment compared to the Holocene non-yedoma area with medians of 5 and 4.5 mg L-1 (p < 0.05), respectively. When yedoma thaw streams with high DOC concentration reach a large yedoma thermokarst lake, we observe an abrupt decrease in DOC concentration, which we attribute to dilution and lake processes such as mineralization. The DOC ages in the large thermokarst lake (between 3,428 and 3,637 C-14 y BP) can be attributed to a mixing of mobilized old yedoma and Holocene carbon. Further downstream after the large thermokarst lake, we find progressively younger DOC ages in the stream water to its mouth, paired with decreasing DOC concentrations. This process could result from dilution with leaching water from Holocene deposits and/or emission of ancient yedoma carbon to the atmosphere. Our study shows that thermokarst lakes and ponds may act as DOC filters, predominantly by diluting incoming waters of higher DOC concentrations or by re-mineralizing DOC to CO2 and CH4. Nevertheless, our results also confirm that the small catchment still contributes DOC on the order of 1.2 kg km(-2) per day from a permafrost landscape with ice-rich yedoma deposits to the Lena River.},
  language  = {en}
}
@article{PerkinsGanzertRojasJimenezetal.2019,
  author    = {Perkins, Anita K. and Ganzert, Lars and Rojas-Jimenez, Keilor and Fonvielle, Jeremy Andre and Hose, Grant C. and Grossart, Hans-Peter},
  title     = {Highly diverse fungal communities in carbon-rich aquifers of two contrasting lakes in Northeast Germany},
  series = {Fungal ecology},
  volume    = {41},
  journal   = {Fungal ecology},
  publisher = {Elsevier},
  address   = {Oxford},
  issn      = {1754-5048},
  doi       = {10.1016/j.funeco.2019.04.004},
  pages     = {116 -- 125},
  year      = {2019},
  abstract  = {Fungi are an important component of microbial communities and are well known for their ability to decompose refractory, highly polymeric organic matter. In soils and aquatic systems, fungi play an important role in carbon processing, however, their diversity, community structure and function as well as ecological role, particularly in groundwater, are poorly studied. The aim of this study was to examine the fungal community composition, diversity and function in groundwater from 16 boreholes located in the vicinity of two lakes in NE Germany that are characterized by contrasting trophic status. The analysis of 28S rRNA gene sequences amplified from the groundwater revealed high fungal diversity arid clear differences in community structure between the aquifers. Most sequences were assigned to Ascomycota and Basidiomycota, but members of Chytridiomycota, Cryptomycota, Zygomycota, Blastocladiomycota, Glomeromycota and Neocallimastigomycota were also detected. In addition, 27 species of fungi were successfully isolated from the groundwater samples and tested for their ability to decompose complex organic polymers - the predominant carbon source in the groundwater. Most isolates showed positive activities for at least one of the tested polymer types, with three strains, belonging to the genera Gibberella, Isaria and Cadophora, able to decompose all tested substrates. Our results highlight the high diversity of fungi in groundwater, and point to their important ecological role in breaking down highly polymeric organic matter in these isolated microbial habitats. (C) 2019 Elsevier Ltd and British Mycological Society. All rights reserved.},
  language  = {en}
}
@phdthesis{Bissinger2003,
  author    = {Bissinger, Vera},
  title     = {Factors determining growth and vertical distribution of planktonic algae in extremely acidic mining lakes (pH 2.7)},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-0000695},
  school      = {Universit{\"a}t Potsdam},
  year      = {2003},
  abstract  = {Die vorliegende Dissertation besch{\"a}ftigt sich mit den Faktoren, die das Wachstum und die Vertikalverteilung von Planktonalgen in extrem sauren Tagebaurestseen (TBS; pH 2-3) beeinflussen. Im exemplarisch untersuchten TBS 111 (pH 2.7; Lausitzer Revier) dominiert die Goldalge Ochromonas sp. in oberen und die Gr{\"u}nalge Chlamydomonas sp. in tieferen Wasserschichten, wobei letztere ein ausgepr{\"a}gtes Tiefenchlorophyll-Maximum (DCM) ausbildet. Es wurde ein deutlicher Einfluss von Limitation durch anorganischen Kohlenstoff (IC) auf das phototrophe Wachstum von Chlamydomonas sp. in oberen Wasserschichten nachgewiesen, die mit zunehmender Tiefe von Lichtlimitation abgel{\"o}st wird. Im Vergleich mit Arbeiten aus neutralen Seen zeigte Chlamydomonas sp. erniedrigte maximale Wachstumsraten, einen gesteigerten Kompensationspunkt und erh{\"o}hte Dunkelrespirationsraten, was auf gesteigerte metabolische Kosten unter den extremen physikalisch-chemischen Bedingungen hinweist. Die Photosyntheseleistungen von Chlamydomonas sp. waren in Starklicht-adaptierten Zellen durch IC-Limitation deutlich verringert. Außerdem ergaben die ermittelten minimalen Zellquoten f{\"u}r Phosphor (P) einen erh{\"o}hten P-Bedarf unter IC-Limitation. Anschließend konnte gezeigt werden, dass Chlamydomonas sp. ein mixotropher Organismus ist, der seine Wachstumsraten {\"u}ber die osmotrophe Aufnahme gel{\"o}sten organischen Kohlenstoffs (DOC) erh{\"o}hen kann. Dadurch ist dieser Organismus f{\"a}hig, in tieferen, Licht-limitierten Wasserschichten zu {\"u}berleben, die einen h{\"o}heren DOC-Gehalt aufweisen. Da die Vertikalverteilung der Algen im TBS 111 jedoch weder durch IC-Limitation, P-Verf{\"u}gbarkeit noch die in situ DOC-Konzentrationen abschließend erkl{\"a}rt werden konnte (bottom-up Kontrolle), wurde eine neue Theorie zur Entstehung der Vertikalverteilung gepr{\"u}ft. Grazing der phagotrophen und phototrophen Alge Ochromonas sp. auf der phototrophen Alge Chlamydomonas sp. erwies sich als herausragender Faktor, der {\"u}ber top-down Kontrolle die Abundanz der Beute in h{\"o}heren Wasserschichten beeinflussen kann. Gemeinsam mit der Tatsache, dass Chlamydomonas sp. DOC zur Wachstumssteigerung verwendet, f{\"u}hrt dies zu einer Akkumulation von Chlamydomonas sp. in der Tiefe, ausgepr{\"a}gt als DCM. Daher erscheint grazing als der Hauptfaktor, der die beobachtete Vertikalschichtung der Algen im TBS 111 hervorruft. Die erzielten Ergebnisse liefern grundlegende Informationen, um die Auswirkungen von Strategien zur Neutralisierung der TBS auf das Nahrungsnetz absch{\"a}tzen zu k{\"o}nnen.},
  language  = {en}
}