Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation
Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Yongjin [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2001 |
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| Schlagwörter: |
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| Anmerkung: |
© Science in China Press 2001 |
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| Übergeordnetes Werk: |
Enthalten in: Science in China / D - Science in China Press, 1996, 44(2001), 1 vom: Jan., Seite 14-23 |
|---|---|
| Übergeordnetes Werk: |
volume:44 ; year:2001 ; number:1 ; month:01 ; pages:14-23 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02906881 |
|---|
| Katalog-ID: |
OLC2063773092 |
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| 520 | |a Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods | ||
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10.1007/BF02906881 doi (DE-627)OLC2063773092 (DE-He213)BF02906881-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Yongjin verfasserin aut Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2001 Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods stalagmite the last glaciation D-O cycle East Asian summer monsoon Wu, Jiangying aut Wu, Jinquan aut Mu, Xinan aut Xu, Hankui aut Chen, Jun aut Enthalten in Science in China / D Science in China Press, 1996 44(2001), 1 vom: Jan., Seite 14-23 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:44 year:2001 number:1 month:01 pages:14-23 https://doi.org/10.1007/BF02906881 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 44 2001 1 01 14-23 |
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10.1007/BF02906881 doi (DE-627)OLC2063773092 (DE-He213)BF02906881-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Yongjin verfasserin aut Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2001 Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods stalagmite the last glaciation D-O cycle East Asian summer monsoon Wu, Jiangying aut Wu, Jinquan aut Mu, Xinan aut Xu, Hankui aut Chen, Jun aut Enthalten in Science in China / D Science in China Press, 1996 44(2001), 1 vom: Jan., Seite 14-23 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:44 year:2001 number:1 month:01 pages:14-23 https://doi.org/10.1007/BF02906881 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 44 2001 1 01 14-23 |
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10.1007/BF02906881 doi (DE-627)OLC2063773092 (DE-He213)BF02906881-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Yongjin verfasserin aut Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2001 Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods stalagmite the last glaciation D-O cycle East Asian summer monsoon Wu, Jiangying aut Wu, Jinquan aut Mu, Xinan aut Xu, Hankui aut Chen, Jun aut Enthalten in Science in China / D Science in China Press, 1996 44(2001), 1 vom: Jan., Seite 14-23 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:44 year:2001 number:1 month:01 pages:14-23 https://doi.org/10.1007/BF02906881 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 44 2001 1 01 14-23 |
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10.1007/BF02906881 doi (DE-627)OLC2063773092 (DE-He213)BF02906881-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Yongjin verfasserin aut Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2001 Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods stalagmite the last glaciation D-O cycle East Asian summer monsoon Wu, Jiangying aut Wu, Jinquan aut Mu, Xinan aut Xu, Hankui aut Chen, Jun aut Enthalten in Science in China / D Science in China Press, 1996 44(2001), 1 vom: Jan., Seite 14-23 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:44 year:2001 number:1 month:01 pages:14-23 https://doi.org/10.1007/BF02906881 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 44 2001 1 01 14-23 |
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10.1007/BF02906881 doi (DE-627)OLC2063773092 (DE-He213)BF02906881-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Yongjin verfasserin aut Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2001 Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods stalagmite the last glaciation D-O cycle East Asian summer monsoon Wu, Jiangying aut Wu, Jinquan aut Mu, Xinan aut Xu, Hankui aut Chen, Jun aut Enthalten in Science in China / D Science in China Press, 1996 44(2001), 1 vom: Jan., Seite 14-23 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:44 year:2001 number:1 month:01 pages:14-23 https://doi.org/10.1007/BF02906881 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 44 2001 1 01 14-23 |
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Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation |
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Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation |
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Wang, Yongjin |
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Science in China / D |
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2001 |
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Wang, Yongjin Wu, Jiangying Wu, Jinquan Mu, Xinan Xu, Hankui Chen, Jun |
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Wang, Yongjin |
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10.1007/BF02906881 |
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correlation between high-resolution climate records from a nanjing stalagmite and grip ice core during the last glaciation |
| title_auth |
Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation |
| abstract |
Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods © Science in China Press 2001 |
| abstractGer |
Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods © Science in China Press 2001 |
| abstract_unstemmed |
Abstract A 400-mm-long stalagmite from Tangshan Cave, Nanjing has been analyzed by a high-precision TIMS-U series dating method and also determined for oxygen and carbon stable isotopic compositions. The results provided a high-resolution paleoclimate record for eastern China during a time interval (from 54 000 to 19 000 aBP) of the last glaciation. The continuous record of oxygen-18 variations in the stalagmite, indicating a precipitation history of the East Asian monsoon, shows not only signals of the Heinrich events, but also the Dansgaard-Oeschger cycles which are first found in the last glacial climate record of the East Asian monsoon area. Although the stalagmite-based climatic signals match well with the GRIP ice core record, some differences between the two records can be recognized: (1) The last glacial climate changes in eastern China exhibited a long-term remarkably cooling trend, superimposed on which were four successive Bond’s cycles illustrated by the $ δ^{18} $O curve. This strong cooling tendency may be an effect of the strong summer monsoon event during the MIS 3 over the Tibetan Plateau. (2) There exist some phase differences of 1000–2000 years between the cooling events in the stalagmite-based climate signal and the GRIP ice core record. Such differences should be further verified by calibrations of multiple dating methods © Science in China Press 2001 |
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Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation |
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