Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene

The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a transition from a global climate state that was 2-3 °C warmer than present with limited ice sheets in the Northern Hemisphere to one that was characterized by continental-scale glaciations at both poles. Growth and dec...

Full description

Saved in:
Bibliographic Details
Main Authors: Patterson, Molly O. (Author) , McKay, R. (Author) , Naish, T. (Author) , Escutia, C. (Author) , Jimenez-Espejo, F. J. (Author) , Raymo, M. E. (Author) , Meyers, S. R. (Author) , Tauxe, L. (Author) , Brinkhuis, H. (Author) , Pross, Jörg (Author)
Format: Article (Journal)
Language:English
Published: 26 October 2014
In: Nature geoscience
Year: 2014, Volume: 7, Issue: 11, Pages: 841-847
ISSN:1752-0908
DOI:10.1038/ngeo2273
Online Access:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1038/ngeo2273
Verlag, lizenzpflichtig, Volltext: https://www.nature.com/articles/ngeo2273
Get full text
Author Notes:M.O. Patterson, R. McKay, T. Naish, C. Escutia, F.J. Jimenez-Espejo, M.E. Raymo, S.R. Meyers, L. Tauxe, H. Brinkhuis and IODP Expedition 318 scientists

MARC

LEADER 00000caa a2200000 c 4500
001 1745059970
003 DE-627
005 20220819081800.0
007 cr uuu---uuuuu
008 210120s2014 xx |||||o 00| ||eng c
024 7 |a 10.1038/ngeo2273  |2 doi 
035 |a (DE-627)1745059970 
035 |a (DE-599)KXP1745059970 
035 |a (OCoLC)1341388979 
040 |a DE-627  |b ger  |c DE-627  |e rda 
041 |a eng 
084 |a 31  |2 sdnb 
100 1 |a Patterson, Molly O.  |e VerfasserIn  |0 (DE-588)1225422728  |0 (DE-627)1745063986  |4 aut 
245 1 0 |a Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene  |c M.O. Patterson, R. McKay, T. Naish, C. Escutia, F.J. Jimenez-Espejo, M.E. Raymo, S.R. Meyers, L. Tauxe, H. Brinkhuis and IODP Expedition 318 scientists 
264 1 |c 26 October 2014 
300 |a 7 
336 |a Text  |b txt  |2 rdacontent 
337 |a Computermedien  |b c  |2 rdamedia 
338 |a Online-Ressource  |b cr  |2 rdacarrier 
500 |a List of authors: A. Klaus, A. Fehr, J.A.P. Bendle, P.K. Bijl, S.M. Bohaty, S.A. Carr, R.B. Dunbar, J.A. Flores, J.J. Gonzalez, T.G. Hayden, M. Iwai, K. Katsuki, G.S. Kong, M. Nakai, M.P. Olney, S. Passchier, S.F. Pekar, J. Pross, C.R. Riesselman, U. Röhl, T. Sakai, P.K. Shrivastava, C.E. Stickley, S. Sugasaki, S. Tuo, T. van de Flierdt, K. Welsh, T. Williams and M. Yamane 
500 |a Gesehen am 20.01.2021 
520 |a The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a transition from a global climate state that was 2-3 °C warmer than present with limited ice sheets in the Northern Hemisphere to one that was characterized by continental-scale glaciations at both poles. Growth and decay of these ice sheets was paced by variations in the Earth’s orbit around the Sun. However, the nature of the influence of orbital forcing on the ice sheets is unclear, particularly in light of the absence of a strong 20,000-year precession signal in geologic records of global ice volume and sea level. Here we present a record of the rate of accumulation of iceberg-rafted debris offshore from the East Antarctic ice sheet, adjacent to the Wilkes Subglacial Basin, between 4.3 and 2.2 million years ago. We infer that maximum iceberg debris accumulation is associated with the enhanced calving of icebergs during ice-sheet margin retreat. In the warmer part of the record, between 4.3 and 3.5 million years ago, spectral analyses show a dominant periodicity of about 40,000 years. Subsequently, the powers of the 100,000-year and 20,000-year signals strengthen. We suggest that, as the Southern Ocean cooled between 3.5 and 2.5 million years ago, the development of a perennial sea-ice field limited the oceanic forcing of the ice sheet. After this threshold was crossed, substantial retreat of the East Antarctic ice sheet occurred only during austral summer insolation maxima, as controlled by the precession cycle. 
700 1 |a McKay, R.  |e VerfasserIn  |4 aut 
700 1 |a Naish, T.  |e VerfasserIn  |4 aut 
700 1 |a Escutia, C.  |e VerfasserIn  |4 aut 
700 1 |a Jimenez-Espejo, F. J.  |e VerfasserIn  |4 aut 
700 1 |a Raymo, M. E.  |e VerfasserIn  |4 aut 
700 1 |a Meyers, S. R.  |e VerfasserIn  |4 aut 
700 1 |a Tauxe, L.  |e VerfasserIn  |4 aut 
700 1 |a Brinkhuis, H.  |e VerfasserIn  |4 aut 
700 1 |a Pross, Jörg  |e VerfasserIn  |0 (DE-588)132619784  |0 (DE-627)690731647  |0 (DE-576)169932028  |4 aut 
773 0 8 |i Enthalten in  |t Nature geoscience  |d London : Nature Publ. Group, 2008  |g 7(2014), 11, Seite 841-847  |h Online-Ressource  |w (DE-627)549589147  |w (DE-600)2396648-8  |w (DE-576)276001060  |x 1752-0908  |7 nnas  |a Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene 
773 1 8 |g volume:7  |g year:2014  |g number:11  |g pages:841-847  |g extent:7  |a Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene 
856 4 0 |u https://doi.org/10.1038/ngeo2273  |x Verlag  |x Resolving-System  |z lizenzpflichtig  |3 Volltext 
856 4 0 |u https://www.nature.com/articles/ngeo2273  |x Verlag  |z lizenzpflichtig  |3 Volltext 
951 |a AR 
992 |a 20210120 
993 |a Article 
994 |a 2014 
998 |g 132619784  |a Pross, Jörg  |m 132619784:Pross, Jörg  |d 120000  |d 121000  |e 120000PP132619784  |e 121000PP132619784  |k 0/120000/  |k 1/120000/121000/  |p 27 
999 |a KXP-PPN1745059970  |e 3839827612 
BIB |a Y 
SER |a journal 
JSO |a {"relHost":[{"disp":"Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early PleistoceneNature geoscience","recId":"549589147","part":{"year":"2014","issue":"11","text":"7(2014), 11, Seite 841-847","extent":"7","pages":"841-847","volume":"7"},"id":{"eki":["549589147"],"zdb":["2396648-8"],"issn":["1752-0908"]},"origin":[{"dateIssuedKey":"2008","publisher":"Nature Publ. Group","dateIssuedDisp":"2008-","publisherPlace":"London"}],"physDesc":[{"extent":"Online-Ressource"}],"pubHistory":["1.2008 -"],"language":["eng"],"type":{"bibl":"periodical","media":"Online-Ressource"},"note":["Gesehen am 12.02.18"],"title":[{"title_sort":"Nature geoscience","title":"Nature geoscience"}]}],"note":["List of authors: A. Klaus, A. Fehr, J.A.P. Bendle, P.K. Bijl, S.M. Bohaty, S.A. Carr, R.B. Dunbar, J.A. Flores, J.J. Gonzalez, T.G. Hayden, M. Iwai, K. Katsuki, G.S. Kong, M. Nakai, M.P. Olney, S. Passchier, S.F. Pekar, J. Pross, C.R. Riesselman, U. Röhl, T. Sakai, P.K. Shrivastava, C.E. Stickley, S. Sugasaki, S. Tuo, T. van de Flierdt, K. Welsh, T. Williams and M. Yamane","Gesehen am 20.01.2021"],"recId":"1745059970","name":{"displayForm":["M.O. Patterson, R. McKay, T. Naish, C. Escutia, F.J. Jimenez-Espejo, M.E. Raymo, S.R. Meyers, L. Tauxe, H. Brinkhuis and IODP Expedition 318 scientists"]},"origin":[{"dateIssuedDisp":"26 October 2014","dateIssuedKey":"2014"}],"id":{"doi":["10.1038/ngeo2273"],"eki":["1745059970"]},"type":{"media":"Online-Ressource","bibl":"article-journal"},"language":["eng"],"physDesc":[{"extent":"7 S."}],"title":[{"title":"Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene","title_sort":"Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene"}],"person":[{"given":"Molly O.","role":"aut","family":"Patterson","display":"Patterson, Molly O."},{"display":"McKay, R.","role":"aut","given":"R.","family":"McKay"},{"family":"Naish","given":"T.","role":"aut","display":"Naish, T."},{"display":"Escutia, C.","given":"C.","role":"aut","family":"Escutia"},{"display":"Jimenez-Espejo, F. J.","role":"aut","given":"F. J.","family":"Jimenez-Espejo"},{"display":"Raymo, M. E.","family":"Raymo","role":"aut","given":"M. E."},{"display":"Meyers, S. R.","given":"S. R.","role":"aut","family":"Meyers"},{"display":"Tauxe, L.","family":"Tauxe","given":"L.","role":"aut"},{"display":"Brinkhuis, H.","given":"H.","role":"aut","family":"Brinkhuis"},{"display":"Pross, Jörg","family":"Pross","given":"Jörg","role":"aut"}]} 
SRT |a PATTERSONMORBITALFOR2620