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2“... (GS-1) over western Europe was governed by coupled ocean and atmospheric changes. However, few works...”
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3by Bartolomé, Miguel, Moreno Caballud, Ana, Sancho Marcén, Carlos, Stoll, Heather, Cacho, Isabel, Spötl, Christoph, Belmonte, Anchel, Edwards, R. Lawrence, Cheng, H., Hellstrom, John“...32 páginas, 3 figuras Greenland Stadial 1 (GS-1) was the last of a long series of severe cooling...”
Published in Proceedings of the National Academy of Sciences (2015)
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4by Peters, Clare, Austin, William Edward Newns, Walden, John, Hibbert, Fiona D.“...)/Greenlancl Stadial (GS) 1 age in northeast Atlantic sediments using rapid, non-destructive magnetic...”
Published in Journal of Quaternary Science (2010)
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5by Peters, Clare, Austin, William Edward Newns, Walden, John, Hibbert, Fiona D.“...)/Greenlancl Stadial (GS) 1 age in northeast Atlantic sediments using rapid, non-destructive magnetic...”
Published in Journal of Quaternary Science (2010)
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6by Fischer, Anders, Mortensen, Morten Fischer, Henriksen, Peter Steen, Mathiassen, Dorte Rørbeck, Olsen, Jesper“... the Greenland ice cores, the occupation can be assigned to the early part of the cold climatic zone GS-1, thus...”
Published in Journal of Archaeological Science (2013)
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7“...The Younger Dryas (GS-1: ~12.9–11.7 ka) constituted a climate reversal, abruptly interrupting...”
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8by Fischer, Anders, Mortensen, Morten Fischer, Henriksen, Peter Steen, Mathiassen, Dorte Rørbeck, Olsen, Jesper“... the Greenland ice cores, the occupation can be assigned to the early part of the cold climatic zone GS-1, thus...”
Published in Journal of Archaeological Science (2013)
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9“... C. The transition from the equivalent of GI-1a into the equivalent of Greenland Stadial (GS) GS-1...”
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10“... C. The transition from the equivalent of GI-1a into the equivalent of Greenland Stadial (GS) GS-1...”
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11“...) and mountain glaciers. This cold reversal, called the Younger Dryas (GS-1: ~12.9–11.7 ka), was responsible...”
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