(Table 1) Gas tie points used to correlate NorthGRIP and Vostol records
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2006
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| _version_ | 1867171825969004544 |
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| author | Landais, Amaëlle Waelbroeck, Claire Masson-Delmotte, Valerie |
| author_facet | Landais, Amaëlle Waelbroeck, Claire Masson-Delmotte, Valerie |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | North Atlantic sediment records (MD95-2042), Greenland (Greenland Ice Core Project (GRIP)) and Antarctica (Byrd and Vostok) ice core climate records have been synchronized over marine isotopic stage 3 (MIS 3) (64 to 24 kyr B.P.) (Shackleton et al., 2000). The resulting common timescale suggested that MD95-2042 d18Obenthic fluctuations were synchronous with temperature changes in Antarctica (dDice or d18Oice records). In order to assess the persistency of this result we have used here the recent Greenland NorthGRIP ice core covering the last glacial inception. We transfer the Antarctic Vostok GT4 timescale to NorthGRIP d18Oice and MD95-2042 d18Oplanktonic records and precisely quantify all the relative timing uncertainties. During the rapid warming of Dansgaard-Oeschger 24, MD95-2042 d18Obenthic decrease is in phase with d18Oplanktonic decrease and therefore with NorthGRIP temperature increase, but it takes place 1700 ± 1100 years after the Antarctic warming. Thus the present study reveals that the results obtained previously for MIS 3 cannot be generalized and demonstrates the need to improve common chronologies for marine and polar archives. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_834990 |
| institution | PANGAEA |
| language | en |
| publishDate | 2006 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Gas tie points used to correlate NorthGRIP and Vostol records Landais, Amaëlle Waelbroeck, Claire Masson-Delmotte, Valerie Age, comment; Age, error; Age model; DEPTH, ice/snow; Greenland; GRIP; GRIP__Campaign; ISTUK; ISTUK electromechanical drill; Sampling/drilling ice North Atlantic sediment records (MD95-2042), Greenland (Greenland Ice Core Project (GRIP)) and Antarctica (Byrd and Vostok) ice core climate records have been synchronized over marine isotopic stage 3 (MIS 3) (64 to 24 kyr B.P.) (Shackleton et al., 2000). The resulting common timescale suggested that MD95-2042 d18Obenthic fluctuations were synchronous with temperature changes in Antarctica (dDice or d18Oice records). In order to assess the persistency of this result we have used here the recent Greenland NorthGRIP ice core covering the last glacial inception. We transfer the Antarctic Vostok GT4 timescale to NorthGRIP d18Oice and MD95-2042 d18Oplanktonic records and precisely quantify all the relative timing uncertainties. During the rapid warming of Dansgaard-Oeschger 24, MD95-2042 d18Obenthic decrease is in phase with d18Oplanktonic decrease and therefore with NorthGRIP temperature increase, but it takes place 1700 ± 1100 years after the Antarctic warming. Thus the present study reveals that the results obtained previously for MIS 3 cannot be generalized and demonstrates the need to improve common chronologies for marine and polar archives. |
| title | (Table 1) Gas tie points used to correlate NorthGRIP and Vostol records |
| topic | Age, comment; Age, error; Age model; DEPTH, ice/snow; Greenland; GRIP; GRIP__Campaign; ISTUK; ISTUK electromechanical drill; Sampling/drilling ice |
| url | https://doi.org/10.1594/PANGAEA.834990 |