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 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. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Poberezhnaya, A. E. [verfasserIn] Fedotov, A. P. [verfasserIn] Sitnikova, T. Ya. [verfasserIn] Semenov, M. Yu. [verfasserIn] Ziborova, G. A. [verfasserIn] Otinova, E. L. [verfasserIn] Khabuev, A. V. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2006

Schlagwörter:	Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake

Übergeordnetes Werk:	Enthalten in: Journal of paleolimnology - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1988, 36(2006), 2 vom: Aug., Seite 133-149
Übergeordnetes Werk:	volume:36 ; year:2006 ; number:2 ; month:08 ; pages:133-149

Links:	Volltext

DOI / URN:	10.1007/s10933-006-0009-3

Katalog-ID:	SPR014728028

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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.
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700	1		\|a Fedotov, A. P. \|e verfasserin \|4 aut
700	1		\|a Sitnikova, T. Ya. \|e verfasserin \|4 aut
700	1		\|a Semenov, M. Yu. \|e verfasserin \|4 aut
700	1		\|a Ziborova, G. A. \|e verfasserin \|4 aut
700	1		\|a Otinova, E. L. \|e verfasserin \|4 aut
700	1		\|a Khabuev, A. V. \|e verfasserin \|4 aut
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matchkey_str	article:15730417:2006----::aeeooiaadaeevrnetleodfhltpesoeeeodfaehbuum
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publishDate	2006
allfields	10.1007/s10933-006-0009-3 doi (DE-627)SPR014728028 (SPR)s10933-006-0009-3-e DE-627 ger DE-627 rakwb eng 560 ASE 930 570 ASE 38.19 bkl 42.93 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 Mongolia (dpeaa)DE-He213 Lake Khubsugul (dpeaa)DE-He213 Ostracod distributions (dpeaa)DE-He213 Bottom sediments (dpeaa)DE-He213 Paleoclimate (dpeaa)DE-He213 Glaciations (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Paleolake (dpeaa)DE-He213 Fedotov, A. P. verfasserin aut Sitnikova, T. Ya. verfasserin aut Semenov, M. Yu. verfasserin aut Ziborova, G. A. verfasserin aut Otinova, E. L. verfasserin aut Khabuev, A. V. verfasserin aut Enthalten in Journal of paleolimnology Dordrecht [u.a.] : Springer Science + Business Media B.V, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)270930205 (DE-600)1478181-5 1573-0417 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://dx.doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-ANG SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.19 ASE 42.93 ASE AR 36 2006 2 08 133-149
spelling	10.1007/s10933-006-0009-3 doi (DE-627)SPR014728028 (SPR)s10933-006-0009-3-e DE-627 ger DE-627 rakwb eng 560 ASE 930 570 ASE 38.19 bkl 42.93 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 Mongolia (dpeaa)DE-He213 Lake Khubsugul (dpeaa)DE-He213 Ostracod distributions (dpeaa)DE-He213 Bottom sediments (dpeaa)DE-He213 Paleoclimate (dpeaa)DE-He213 Glaciations (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Paleolake (dpeaa)DE-He213 Fedotov, A. P. verfasserin aut Sitnikova, T. Ya. verfasserin aut Semenov, M. Yu. verfasserin aut Ziborova, G. A. verfasserin aut Otinova, E. L. verfasserin aut Khabuev, A. V. verfasserin aut Enthalten in Journal of paleolimnology Dordrecht [u.a.] : Springer Science + Business Media B.V, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)270930205 (DE-600)1478181-5 1573-0417 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://dx.doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-ANG SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.19 ASE 42.93 ASE AR 36 2006 2 08 133-149
allfields_unstemmed	10.1007/s10933-006-0009-3 doi (DE-627)SPR014728028 (SPR)s10933-006-0009-3-e DE-627 ger DE-627 rakwb eng 560 ASE 930 570 ASE 38.19 bkl 42.93 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 Mongolia (dpeaa)DE-He213 Lake Khubsugul (dpeaa)DE-He213 Ostracod distributions (dpeaa)DE-He213 Bottom sediments (dpeaa)DE-He213 Paleoclimate (dpeaa)DE-He213 Glaciations (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Paleolake (dpeaa)DE-He213 Fedotov, A. P. verfasserin aut Sitnikova, T. Ya. verfasserin aut Semenov, M. Yu. verfasserin aut Ziborova, G. A. verfasserin aut Otinova, E. L. verfasserin aut Khabuev, A. V. verfasserin aut Enthalten in Journal of paleolimnology Dordrecht [u.a.] : Springer Science + Business Media B.V, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)270930205 (DE-600)1478181-5 1573-0417 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://dx.doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-ANG SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.19 ASE 42.93 ASE AR 36 2006 2 08 133-149
allfieldsGer	10.1007/s10933-006-0009-3 doi (DE-627)SPR014728028 (SPR)s10933-006-0009-3-e DE-627 ger DE-627 rakwb eng 560 ASE 930 570 ASE 38.19 bkl 42.93 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 Mongolia (dpeaa)DE-He213 Lake Khubsugul (dpeaa)DE-He213 Ostracod distributions (dpeaa)DE-He213 Bottom sediments (dpeaa)DE-He213 Paleoclimate (dpeaa)DE-He213 Glaciations (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Paleolake (dpeaa)DE-He213 Fedotov, A. P. verfasserin aut Sitnikova, T. Ya. verfasserin aut Semenov, M. Yu. verfasserin aut Ziborova, G. A. verfasserin aut Otinova, E. L. verfasserin aut Khabuev, A. V. verfasserin aut Enthalten in Journal of paleolimnology Dordrecht [u.a.] : Springer Science + Business Media B.V, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)270930205 (DE-600)1478181-5 1573-0417 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://dx.doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-ANG SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.19 ASE 42.93 ASE AR 36 2006 2 08 133-149
allfieldsSound	10.1007/s10933-006-0009-3 doi (DE-627)SPR014728028 (SPR)s10933-006-0009-3-e DE-627 ger DE-627 rakwb eng 560 ASE 930 570 ASE 38.19 bkl 42.93 bkl 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 Computermedien c rdamedia Online-Ressource cr rdacarrier 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 (dpeaa)DE-He213 Mongolia (dpeaa)DE-He213 Lake Khubsugul (dpeaa)DE-He213 Ostracod distributions (dpeaa)DE-He213 Bottom sediments (dpeaa)DE-He213 Paleoclimate (dpeaa)DE-He213 Glaciations (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Paleolake (dpeaa)DE-He213 Fedotov, A. P. verfasserin aut Sitnikova, T. Ya. verfasserin aut Semenov, M. Yu. verfasserin aut Ziborova, G. A. verfasserin aut Otinova, E. L. verfasserin aut Khabuev, A. V. verfasserin aut Enthalten in Journal of paleolimnology Dordrecht [u.a.] : Springer Science + Business Media B.V, 1988 36(2006), 2 vom: Aug., Seite 133-149 (DE-627)270930205 (DE-600)1478181-5 1573-0417 nnns volume:36 year:2006 number:2 month:08 pages:133-149 https://dx.doi.org/10.1007/s10933-006-0009-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-ANG SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.19 ASE 42.93 ASE AR 36 2006 2 08 133-149
language	English
source	Enthalten in Journal of paleolimnology 36(2006), 2 vom: Aug., Seite 133-149 volume:36 year:2006 number:2 month:08 pages:133-149
sourceStr	Enthalten in Journal of paleolimnology 36(2006), 2 vom: Aug., Seite 133-149 volume:36 year:2006 number:2 month:08 pages:133-149
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Central Asia Mongolia Lake Khubsugul Ostracod distributions Bottom sediments Paleoclimate Glaciations Late Pleistocene Paleolake
dewey-raw	560
isfreeaccess_bool	false
container_title	Journal of paleolimnology
authorswithroles_txt_mv	Poberezhnaya, A. E. @@aut@@ Fedotov, A. P. @@aut@@ Sitnikova, T. Ya. @@aut@@ Semenov, M. Yu. @@aut@@ Ziborova, G. A. @@aut@@ Otinova, E. L. @@aut@@ Khabuev, A. V. @@aut@@
publishDateDaySort_date	2006-08-01T00:00:00Z
hierarchy_top_id	270930205
dewey-sort	3560
id	SPR014728028
language_de	englisch
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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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</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. 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. 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author	Poberezhnaya, A. E.
spellingShingle	Poberezhnaya, A. E. ddc 560 ddc 930 bkl 38.19 bkl 42.93 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
authorStr	Poberezhnaya, A. E.
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topic_title	560 ASE 930 570 ASE 38.19 bkl 42.93 bkl Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains Central Asia (dpeaa)DE-He213 Mongolia (dpeaa)DE-He213 Lake Khubsugul (dpeaa)DE-He213 Ostracod distributions (dpeaa)DE-He213 Bottom sediments (dpeaa)DE-He213 Paleoclimate (dpeaa)DE-He213 Glaciations (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Paleolake (dpeaa)DE-He213
topic	ddc 560 ddc 930 bkl 38.19 bkl 42.93 misc Central Asia misc Mongolia misc Lake Khubsugul misc Ostracod distributions misc Bottom sediments misc Paleoclimate misc Glaciations misc Late Pleistocene misc Paleolake
topic_unstemmed	ddc 560 ddc 930 bkl 38.19 bkl 42.93 misc Central Asia misc Mongolia misc Lake Khubsugul misc Ostracod distributions misc Bottom sediments misc Paleoclimate misc Glaciations misc Late Pleistocene misc Paleolake
topic_browse	ddc 560 ddc 930 bkl 38.19 bkl 42.93 misc Central Asia misc Mongolia misc Lake Khubsugul misc Ostracod distributions misc Bottom sediments misc Paleoclimate misc Glaciations misc Late Pleistocene misc Paleolake
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title	Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains
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title_full	Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains
author_sort	Poberezhnaya, A. E.
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author_browse	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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author-letter	Poberezhnaya, A. E.
doi_str_mv	10.1007/s10933-006-0009-3
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title_sort	paleoecological and paleoenvironmental record of the late pleistocene record of lake khubsugul (mongolia) based on ostracod remains
title_auth	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.
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.
abstract_unstemmed	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.
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title_short	Paleoecological and paleoenvironmental record of the Late Pleistocene record of Lake Khubsugul (Mongolia) based on ostracod remains
url	https://dx.doi.org/10.1007/s10933-006-0009-3
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author2	Fedotov, A. P. Sitnikova, T. Ya Semenov, M. Yu Ziborova, G. A. Otinova, E. L. Khabuev, A. V.
author2Str	Fedotov, A. P. Sitnikova, T. Ya Semenov, M. Yu Ziborova, G. A. Otinova, E. L. Khabuev, A. V.
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doi_str	10.1007/s10933-006-0009-3
up_date	2024-07-04T02:50:36.438Z
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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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