Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A.
Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains....
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Xia, J. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1997 |
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| Schlagwörter: |
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| Anmerkung: |
© Kluwer Academic Publishers 1997 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of paleolimnology - Kluwer Academic Publishers, 1988, 17(1997), 1 vom: Jan., Seite 85-100 |
|---|---|
| Übergeordnetes Werk: |
volume:17 ; year:1997 ; number:1 ; month:01 ; pages:85-100 |
| Links: |
|---|
| DOI / URN: |
10.1023/A:1007921328712 |
|---|
| Katalog-ID: |
OLC2071079167 |
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| 245 | 1 | 0 | |a Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. |
| 264 | 1 | |c 1997 | |
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| 520 | |a Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. | ||
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| 700 | 1 | |a Engstrom, D. R. |4 aut | |
| 700 | 1 | |a Ito, E. |4 aut | |
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10.1023/A:1007921328712 doi (DE-627)OLC2071079167 (DE-He213)A:1007921328712-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Xia, J. verfasserin aut Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. Calcite Holocene Ostracode Temperature Oscillation Holocene Climate Haskell, B. J. aut Engstrom, D. R. aut Ito, E. aut Enthalten in Journal of paleolimnology Kluwer Academic Publishers, 1988 17(1997), 1 vom: Jan., Seite 85-100 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:17 year:1997 number:1 month:01 pages:85-100 https://doi.org/10.1023/A:1007921328712 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_4012 AR 17 1997 1 01 85-100 |
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10.1023/A:1007921328712 doi (DE-627)OLC2071079167 (DE-He213)A:1007921328712-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Xia, J. verfasserin aut Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. Calcite Holocene Ostracode Temperature Oscillation Holocene Climate Haskell, B. J. aut Engstrom, D. R. aut Ito, E. aut Enthalten in Journal of paleolimnology Kluwer Academic Publishers, 1988 17(1997), 1 vom: Jan., Seite 85-100 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:17 year:1997 number:1 month:01 pages:85-100 https://doi.org/10.1023/A:1007921328712 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_4012 AR 17 1997 1 01 85-100 |
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10.1023/A:1007921328712 doi (DE-627)OLC2071079167 (DE-He213)A:1007921328712-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Xia, J. verfasserin aut Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. Calcite Holocene Ostracode Temperature Oscillation Holocene Climate Haskell, B. J. aut Engstrom, D. R. aut Ito, E. aut Enthalten in Journal of paleolimnology Kluwer Academic Publishers, 1988 17(1997), 1 vom: Jan., Seite 85-100 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:17 year:1997 number:1 month:01 pages:85-100 https://doi.org/10.1023/A:1007921328712 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_4012 AR 17 1997 1 01 85-100 |
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10.1023/A:1007921328712 doi (DE-627)OLC2071079167 (DE-He213)A:1007921328712-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Xia, J. verfasserin aut Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. Calcite Holocene Ostracode Temperature Oscillation Holocene Climate Haskell, B. J. aut Engstrom, D. R. aut Ito, E. aut Enthalten in Journal of paleolimnology Kluwer Academic Publishers, 1988 17(1997), 1 vom: Jan., Seite 85-100 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:17 year:1997 number:1 month:01 pages:85-100 https://doi.org/10.1023/A:1007921328712 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_4012 AR 17 1997 1 01 85-100 |
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10.1023/A:1007921328712 doi (DE-627)OLC2071079167 (DE-He213)A:1007921328712-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Xia, J. verfasserin aut Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. Calcite Holocene Ostracode Temperature Oscillation Holocene Climate Haskell, B. J. aut Engstrom, D. R. aut Ito, E. aut Enthalten in Journal of paleolimnology Kluwer Academic Publishers, 1988 17(1997), 1 vom: Jan., Seite 85-100 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:17 year:1997 number:1 month:01 pages:85-100 https://doi.org/10.1023/A:1007921328712 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_4012 AR 17 1997 1 01 85-100 |
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Xia, J. ddc 570 ssgn 14 misc Calcite misc Holocene misc Ostracode misc Temperature Oscillation misc Holocene Climate Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. |
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570 930 VZ 14 13 12 ssgn Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. Calcite Holocene Ostracode Temperature Oscillation Holocene Climate |
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Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. |
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Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. |
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Xia, J. Haskell, B. J. Engstrom, D. R. Ito, E. |
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holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from coldwater lake, north dakota, u.s.a. |
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Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, U.S.A. |
| abstract |
Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. © Kluwer Academic Publishers 1997 |
| abstractGer |
Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. © Kluwer Academic Publishers 1997 |
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Abstract The geochemistry of ostracode shells and bulk carbonates in a 19-meter sediment core documents at century-scale resolution the evolution of water chemistry in Coldwater Lake, North Dakota, providing a continuous paleohydrologic record of Holocene climate change in the northern Great Plains. A combination of $ δ^{18} $O, $ δ^{13} $C, Mg/Ca and Sr/Ca in ostracode calcite aided by Sr/Ca in bulk carbonates are used to constrain the paleoclimatic reconstructions. A fresh-water phase in the early Holocene, indicated by the absence of Candona rawsoni and low concentrations of Sr/Ca in bulk carbonate, was followed by a sharp increase in salinity between 10 800 and 8900 yr B.P. The climate was predominately dry during the late part of the early Holocene and most of the middle Holocene (8900–5000 yr B.P.), when the lake was very sensitive and recorded a series of dry and wet oscillations. Maximum salinity occurred around 5500 yr B.P. and was followed by a gradual decrease between 5000 and 2400 yr B.P. From 2400 yr B.P. the $ δ^{18} $O, Mg/Ca, and Sr/Ca in the ostracodes indicate generally wet conditions interrupted by a series of lesser salinity and temperature oscillations lasting until 600 yr B.P. Ostracode geochemistry indicates that a warm and dry climate returned at about the time of the Little Ice Age (600–150 yr B.P.). Ostracode $ δ^{13} $C shows a ong-term increasing trend during the Holocene, which suggests that lake productivity and atmospheric $ CO_{2} $ exchange made greater contributions to the hypolimnetic carbon pool as the lake became shallower with time. © Kluwer Academic Publishers 1997 |
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