author_facet Fleitmann, D.
Cheng, H.
Badertscher, S.
Edwards, R. L.
Mudelsee, M.
Göktürk, O. M.
Fankhauser, A.
Pickering, R.
Raible, C. C.
Matter, A.
Kramers, J.
Tüysüz, O.
Fleitmann, D.
Cheng, H.
Badertscher, S.
Edwards, R. L.
Mudelsee, M.
Göktürk, O. M.
Fankhauser, A.
Pickering, R.
Raible, C. C.
Matter, A.
Kramers, J.
Tüysüz, O.
author Fleitmann, D.
Cheng, H.
Badertscher, S.
Edwards, R. L.
Mudelsee, M.
Göktürk, O. M.
Fankhauser, A.
Pickering, R.
Raible, C. C.
Matter, A.
Kramers, J.
Tüysüz, O.
spellingShingle Fleitmann, D.
Cheng, H.
Badertscher, S.
Edwards, R. L.
Mudelsee, M.
Göktürk, O. M.
Fankhauser, A.
Pickering, R.
Raible, C. C.
Matter, A.
Kramers, J.
Tüysüz, O.
Geophysical Research Letters
Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
General Earth and Planetary Sciences
Geophysics
author_sort fleitmann, d.
spelling Fleitmann, D. Cheng, H. Badertscher, S. Edwards, R. L. Mudelsee, M. Göktürk, O. M. Fankhauser, A. Pickering, R. Raible, C. C. Matter, A. Kramers, J. Tüysüz, O. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2009gl040050 <jats:p>A 50 kyr‐long exceptionally well‐dated and highly resolved stalagmite oxygen (<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O) and carbon (<jats:italic>δ</jats:italic><jats:sup>13</jats:sup>C) isotope record from Sofular Cave in northwestern Turkey helps to further improve the dating of Greenland Interstadials (GI) 1, and 3–12. Timing of most GI in the Sofular record is consistent within ±10 to 300 years with the “iconic” Hulu Cave record. Larger divergences (&gt;500 years) between Sofular and Hulu are only observed for GI 4 and 7. The Sofular record differs from the most recent NGRIP chronology by up to several centuries, whereas age offsets do not increase systematically with depth. The Sofular record also reveals a rapid and sensitive climate and ecosystem response in the eastern Mediterranean to GI, whereas a phase lag of ∼100 years between climate and full ecosystem response is evident. Finally, results of spectral analyses of the Sofular isotope records do not support a 1,470‐year pacing of GI.</jats:p> Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey Geophysical Research Letters
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series Geophysical Research Letters
source_id 49
title Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_unstemmed Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_full Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_fullStr Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_full_unstemmed Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_short Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_sort timing and climatic impact of greenland interstadials recorded in stalagmites from northern turkey
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/2009gl040050
publishDate 2009
physical
description <jats:p>A 50 kyr‐long exceptionally well‐dated and highly resolved stalagmite oxygen (<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O) and carbon (<jats:italic>δ</jats:italic><jats:sup>13</jats:sup>C) isotope record from Sofular Cave in northwestern Turkey helps to further improve the dating of Greenland Interstadials (GI) 1, and 3–12. Timing of most GI in the Sofular record is consistent within ±10 to 300 years with the “iconic” Hulu Cave record. Larger divergences (&gt;500 years) between Sofular and Hulu are only observed for GI 4 and 7. The Sofular record differs from the most recent NGRIP chronology by up to several centuries, whereas age offsets do not increase systematically with depth. The Sofular record also reveals a rapid and sensitive climate and ecosystem response in the eastern Mediterranean to GI, whereas a phase lag of ∼100 years between climate and full ecosystem response is evident. Finally, results of spectral analyses of the Sofular isotope records do not support a 1,470‐year pacing of GI.</jats:p>
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author Fleitmann, D., Cheng, H., Badertscher, S., Edwards, R. L., Mudelsee, M., Göktürk, O. M., Fankhauser, A., Pickering, R., Raible, C. C., Matter, A., Kramers, J., Tüysüz, O.
author_facet Fleitmann, D., Cheng, H., Badertscher, S., Edwards, R. L., Mudelsee, M., Göktürk, O. M., Fankhauser, A., Pickering, R., Raible, C. C., Matter, A., Kramers, J., Tüysüz, O., Fleitmann, D., Cheng, H., Badertscher, S., Edwards, R. L., Mudelsee, M., Göktürk, O. M., Fankhauser, A., Pickering, R., Raible, C. C., Matter, A., Kramers, J., Tüysüz, O.
author_sort fleitmann, d.
container_issue 19
container_start_page 0
container_title Geophysical Research Letters
container_volume 36
description <jats:p>A 50 kyr‐long exceptionally well‐dated and highly resolved stalagmite oxygen (<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O) and carbon (<jats:italic>δ</jats:italic><jats:sup>13</jats:sup>C) isotope record from Sofular Cave in northwestern Turkey helps to further improve the dating of Greenland Interstadials (GI) 1, and 3–12. Timing of most GI in the Sofular record is consistent within ±10 to 300 years with the “iconic” Hulu Cave record. Larger divergences (&gt;500 years) between Sofular and Hulu are only observed for GI 4 and 7. The Sofular record differs from the most recent NGRIP chronology by up to several centuries, whereas age offsets do not increase systematically with depth. The Sofular record also reveals a rapid and sensitive climate and ecosystem response in the eastern Mediterranean to GI, whereas a phase lag of ∼100 years between climate and full ecosystem response is evident. Finally, results of spectral analyses of the Sofular isotope records do not support a 1,470‐year pacing of GI.</jats:p>
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spelling Fleitmann, D. Cheng, H. Badertscher, S. Edwards, R. L. Mudelsee, M. Göktürk, O. M. Fankhauser, A. Pickering, R. Raible, C. C. Matter, A. Kramers, J. Tüysüz, O. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2009gl040050 <jats:p>A 50 kyr‐long exceptionally well‐dated and highly resolved stalagmite oxygen (<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O) and carbon (<jats:italic>δ</jats:italic><jats:sup>13</jats:sup>C) isotope record from Sofular Cave in northwestern Turkey helps to further improve the dating of Greenland Interstadials (GI) 1, and 3–12. Timing of most GI in the Sofular record is consistent within ±10 to 300 years with the “iconic” Hulu Cave record. Larger divergences (&gt;500 years) between Sofular and Hulu are only observed for GI 4 and 7. The Sofular record differs from the most recent NGRIP chronology by up to several centuries, whereas age offsets do not increase systematically with depth. The Sofular record also reveals a rapid and sensitive climate and ecosystem response in the eastern Mediterranean to GI, whereas a phase lag of ∼100 years between climate and full ecosystem response is evident. Finally, results of spectral analyses of the Sofular isotope records do not support a 1,470‐year pacing of GI.</jats:p> Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey Geophysical Research Letters
spellingShingle Fleitmann, D., Cheng, H., Badertscher, S., Edwards, R. L., Mudelsee, M., Göktürk, O. M., Fankhauser, A., Pickering, R., Raible, C. C., Matter, A., Kramers, J., Tüysüz, O., Geophysical Research Letters, Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey, General Earth and Planetary Sciences, Geophysics
title Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_full Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_fullStr Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_full_unstemmed Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_short Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
title_sort timing and climatic impact of greenland interstadials recorded in stalagmites from northern turkey
title_unstemmed Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/2009gl040050