Lacustrine systems of Clearwater Mesa (James Ross Island, north-eastern Antarctic Peninsula): geomorphological setting and limnological characterization

0509968 - BC 2020 RIV GB eng J - Článek v odborném periodiku
Roman, M. - Nedbalová, L. - Kohler, T. J. - Lirio, J.M. - Coria, S.H. - Kopáček, Jiří - Vignoni, P. A. - Kopalová, K. - Lecomte, K. L. - Elster, J. - Nývlt, D.
Lacustrine systems of Clearwater Mesa (James Ross Island, north-eastern Antarctic Peninsula): geomorphological setting and limnological characterization.
Antarctic Science. Roč. 31, č. 4 (2019), s. 169-188. ISSN 0954-1020. E-ISSN 1365-2079
Institucionální podpora: RVO:60077344
Klíčová slova: deglaciation * hydrology * lake origin * lake typology * landscape evolution
Obor OECD: Water resources
Impakt faktor: 1.417, rok: 2019
Způsob publikování: Omezený přístup
https://www.cambridge.org/core/journals/antarctic-science/article/lacustrine-systems-of-clearwater-mesa-james-ross-island-northeastern-antarctic-peninsula-geomorphological-setting-and-limnological-characterization/91EEB3EBD354FD8F7D1B2AA3C0B89A84

Lentic freshwater habitats are important centres of biodiversity within the infrequent ice-free oases across Antarctica. Given imminent climate changes, it is crucial to catalogue these habitats in order to provide baseline data for future monitoring and biological surveys. The lacustrine systems of Clearwater Mesa, a previously unexplored part of James Ross Island, north-eastern Antarctic Peninsula, are described here. We conducted basic geomorphological and limnological surveys over three Antarctic summers (2009-16) to characterize landscape evolution, infer the origin of lake basins and assess the variability in their water chemistry. Stable shallow lakes, formed in depressions between lava tumuli following the last deglaciation, were found to dominate the volcanic mesa, although several peripheral lakes in ice-proximal settings appear to have formed recently as a result of post-Neoglacial ice recession. We found large heterogeneity in conductivity (similar to 10-7000 mu S cm(-1)), despite the lithologically uniform substrate. This variability was shown to be related to lake type, basin type (open vs closed), meltwater source and proximity to the coast. Inter-annual differences were attributed to changes in sea spray influx and snow accumulation driven by variable weather conditions. Overall, the ion composition of lakes suggested that sea spray was the dominant source of ions, followed by the weathering of bedrock.
Trvalý link: http://hdl.handle.net/11104/0300549