Late Pleistocene to Holocene Palaeohydrological History of the Thermal-Spring-Fed Lake Pețea (NW Romania) Revealed by Radiocarbon Dating and Complex Sedimentological Investigations

Dados Bibliográficos

ID15801751
AutoresSándor Gulyá (0000-0002-3384-2381, University of Szeged, autor correspondente), Sándor Gulyás (University of Szeged), Pál Sümegi (0000-0003-1755-4440, University of Szeged)
Ano2023
Volume6
Fascículo2
Páginas37-37
Data de publicação2023-06-12
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoQuaternary (JOURNAL)
Identificadores do periódicoISSN: 2571-550X • E-ISSN: 2571-550X
EditoraMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/quat6020037
OpenAlexW4380632531
IdiomaEN
Referências citadas59

Understanding sedimentation processes in response to past hydrogeological and climatic changes and capturing millennial-scale variations is a key focus of lacustrine paleoenvironmental research. This study presents the first high-resolution chronology and sedimentary data for the small thermal-spring-fed Lake Pețea, NW Romania, and unravels the evolutionary history of the lake harboring a unique endemic fauna. Its small size and single source of water make it particularly sensitive to hydrological changes. In the recent past, over-exploitation of the thermal water has led to the complete drying up of the lake and the extinction of its fauna. Nevertheless, past spatio-temporal variation of environmental factors, in particular the fluctuation of lake levels and water temperature, must have had a significant impact on the survival and evolution of the endemic mollusk fauna. This fact makes this study particularly important. Based on our results, a three-stage sedimentary evolution occurred, mainly controlled by major climate-driven hydrological changes also seen in regional records, i.e., 17.5–14.5 ka shallow eutrophic lake, 14.5–5.5 ka oligotrophic carbonate-rich lake, and 5.5–0.5 ka shallow eutrophic lake. A major lowstand at 11.7–10.2 ka due to drier climate was followed by progressively rising water levels up to 5 ka followed by a drop. The main control on lake level fluctuations and sedimentary phases was the varying input of thermal water due to recurring increased/decreased recharge of the underground shallow karst water system. The driving factor of thermal water discharge was different during the Late Glacial than the Holocene. It was the warming of the climate at 14.5 ka cal BP and melting of regional ice sheets in addition to increased precipitation that created an oligotrophic lake by recharging the underground thermal water system. Conversely, during the Holocene, increasing/decreasing moisture availability driven by major climate forcings was in control of thermal water recharge, erosion, and fluctuating lake levels

Fauna · Geography · Glacial period · Holocene · Hydrology (agriculture · Paleolimnology · Physical geography · Pleistocene · Radiocarbon dating · Sedimentary rock · Spring (device · Stage (stratigraphy · Water level · Geology and Paleoclimatology Research · Karst Systems and Hydrogeology · Marine and environmental studies · Ecology · Geology · Paleontology