Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains
Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obta...
Ausführliche Beschreibung
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| Autor*in: |
Poberezhnaya, A. E. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2006 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media B.V. 2006 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of paleolimnology - Springer Netherlands, 1988, 36(2006), 2 vom: Aug., Seite 133-149 |
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| Übergeordnetes Werk: |
volume:36 ; year:2006 ; number:2 ; month:08 ; pages:133-149 |
| Links: |
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| DOI / URN: |
10.1007/s10933-006-0009-3 |
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OLC2071086503 |
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| 245 | 1 | 0 | |a Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains |
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| 520 | |a Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. | ||
| 650 | 4 | |a Central Asia | |
| 650 | 4 | |a Mongolia | |
| 650 | 4 | |a Lake Khubsugul | |
| 650 | 4 | |a Ostracod distributions | |
| 650 | 4 | |a Bottom sediments | |
| 650 | 4 | |a Paleoclimate | |
| 650 | 4 | |a Glaciations | |
| 650 | 4 | |a Late Pleistocene | |
| 650 | 4 | |a Paleolake | |
| 700 | 1 | |a Fedotov, A. P. |4 aut | |
| 700 | 1 | |a Sitnikova, T. Ya. |4 aut | |
| 700 | 1 | |a Semenov, M. Yu. |4 aut | |
| 700 | 1 | |a Ziborova, G. A. |4 aut | |
| 700 | 1 | |a Otinova, E. L. |4 aut | |
| 700 | 1 | |a Khabuev, A. V. |4 aut | |
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10.1007/s10933-006-0009-3 doi (DE-627)OLC2071086503 (DE-He213)s10933-006-0009-3-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Poberezhnaya, A. E. verfasserin aut Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2006 Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake Fedotov, A. P. aut Sitnikova, T. Ya. aut Semenov, M. Yu. aut Ziborova, G. A. aut Otinova, E. L. aut Khabuev, A. V. aut Enthalten in Journal of paleolimnology Springer Netherlands, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 36 2006 2 08 133-149 |
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10.1007/s10933-006-0009-3 doi (DE-627)OLC2071086503 (DE-He213)s10933-006-0009-3-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Poberezhnaya, A. E. verfasserin aut Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2006 Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake Fedotov, A. P. aut Sitnikova, T. Ya. aut Semenov, M. Yu. aut Ziborova, G. A. aut Otinova, E. L. aut Khabuev, A. V. aut Enthalten in Journal of paleolimnology Springer Netherlands, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 36 2006 2 08 133-149 |
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10.1007/s10933-006-0009-3 doi (DE-627)OLC2071086503 (DE-He213)s10933-006-0009-3-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Poberezhnaya, A. E. verfasserin aut Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2006 Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake Fedotov, A. P. aut Sitnikova, T. Ya. aut Semenov, M. Yu. aut Ziborova, G. A. aut Otinova, E. L. aut Khabuev, A. V. aut Enthalten in Journal of paleolimnology Springer Netherlands, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 36 2006 2 08 133-149 |
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10.1007/s10933-006-0009-3 doi (DE-627)OLC2071086503 (DE-He213)s10933-006-0009-3-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Poberezhnaya, A. E. verfasserin aut Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2006 Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake Fedotov, A. P. aut Sitnikova, T. Ya. aut Semenov, M. Yu. aut Ziborova, G. A. aut Otinova, E. L. aut Khabuev, A. V. aut Enthalten in Journal of paleolimnology Springer Netherlands, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 36 2006 2 08 133-149 |
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10.1007/s10933-006-0009-3 doi (DE-627)OLC2071086503 (DE-He213)s10933-006-0009-3-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Poberezhnaya, A. E. verfasserin aut Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2006 Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake Fedotov, A. P. aut Sitnikova, T. Ya. aut Semenov, M. Yu. aut Ziborova, G. A. aut Otinova, E. L. aut Khabuev, A. V. aut Enthalten in Journal of paleolimnology Springer Netherlands, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 36 2006 2 08 133-149 |
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E.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media B.V. 2006</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. 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Poberezhnaya, A. E. ddc 570 ssgn 14 misc Central Asia misc Mongolia misc Lake Khubsugul misc Ostracod distributions misc Bottom sediments misc Paleoclimate misc Glaciations misc Late Pleistocene misc Paleolake Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains |
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570 930 VZ 14 13 12 ssgn Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake |
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Poberezhnaya, A. E. Fedotov, A. P. Sitnikova, T. Ya. Semenov, M. Yu. Ziborova, G. A. Otinova, E. L. Khabuev, A. V. |
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paleoecological and paleoenvironmental record of the late pleistocene record of lake khubsugul (mongolia) based on ostracod remains |
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Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains |
| abstract |
Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. © Springer Science+Business Media B.V. 2006 |
| abstractGer |
Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. © Springer Science+Business Media B.V. 2006 |
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Abstract This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. © Springer Science+Business Media B.V. 2006 |
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