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221by Whittington, Graeme, Buckland, Paul, Edwards, Kevin. J., Greenwood, Malcolm, Hall, Adrian M., Robinson, Marie“... stratigraphical event GI‐1. Event GS‐1 is revealed by the non‐pollen evidence, especially by Coleoptera...”
Published in Journal of Quaternary Science (2003)
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222“... record, including the (Younger Dryas) cooling event from GI‐1a to GS‐1 beginning c. 12650 GRIP yr BP Some...”
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223by Gedminienė, Laura“... poor pioneer vegetation changed to the pine forest, and the GS-1 event with the spread of tundra-type...”
Published 2020
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224by Druzhinina, Olga, Subetto, Dmitry, Stančikaitė, Miglė, Vaikutienė, Giedrė, Kublitsky, Jury, Arslanov, Khikmatulla“... of the environmental regime enabled birch and pine woods to spread during the second part of the GS-1 event...”
Published in Baltica (2015)
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225by Druzhinina, Olga, Subetto, Dmitry, Stančikaitė, Miglė, Vaikutienė, Giedrė, Kublitsky, Jury, Arslanov, Khikmatulla“... of the environmental regime enabled birch and pine woods to spread during the second part of the GS-1 event...”
Published in Baltica (2015)
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226by Gedminienė, Laura“... poor pioneer vegetation changed to the pine forest, and the GS-1 event with the spread of tundra-type...”
Published 2020
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227“... the rate of regression slowed during the Younger Dryas interval (GS-1). The lowest shoreline...”
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229by SMALL, DAVID, AUSTIN, WILLIAM, RINTERKNECHT, VINCENT“... Dryas (GS‐1) cooling episode. The general absence of IRD at southern locations at other times during GI...”
Published in Journal of Quaternary Science (2013)
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230by WASTEGÅRD, STEFAN, TURNEY, CHRIS S. M., LOWE, J. JOHN, ROBERTS, STEPHEN J.“... Dryas chronozone or GS‐1 event of the GRIP stratigraphy. Until recently, the known distribution of wind...”
Published in Boreas (2000)
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231by MacLeod, A., Palmer, A., Lowe, J., Rose, J., Bryant, C.L., Merritt, J.“... transitions that, on evidence from Greenland ice cores, lasted from 12.85 until 11.65 ka cal BP (GS-1...”
Published in Global and Planetary Change (2011)
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232by MacLeod, Alison, Palmer, Adrian, Lowe, John, Rose, James, Bryant, Charlotte, Merritt, Jonathan“... transitions that, on evidence from Greenland ice cores, lasted from 12.85 until 11.65 ka cal BP (GS-1...”
Published in Global and Planetary Change (2011)
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233“... ca. 14 kyr BP, but there is evidence of ice rafting up to the end of the GS-1 (Greenland Stadial 1...”
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234“... Dryas (GS-1) cooling episode. The general absence of IRD at southern locations at other times during GI...”
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235“... (11.7) ka BP indicate a cold and dry climate during the Younger Dryas (GS-1). During the Early Holocene...”
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236“... Dryas (GS-1) cooling episode. The general absence of IRD at southern locations at other times during GI...”
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237“... provided over GS-1 (roughly equivalent to the Younger Dryas) and GI-1 (roughly equivalent to the Bølling...”
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238by 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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239by Bjorck, Svante, Walker, Michael J.C., Cwynar, Les C., Johnsen, Sigfus, Knudsen, Karen-Luise, Lowe, J. John, Wohlfarth, Barbara“... episodes, Greenland Stadials 1 (GS-1) and 2 (GS-2), and two interstadial events, Greenland Interstadials 1...”
Published 1998
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240“...With the exception of the GS-1/Younger Dryas cold period marine reservoir ages for the Last...”
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