Synchronisation of palaeoenvironmental events in the North Atlantic region during the Last Termination: a revised protocol recommended by the INTIMATE group

Lowe, John J.; Rasmussen, S. O.; Björck, Svante; Hoek, Wim Z.; Steffensen, Jørgen Peder; Walker, M. J. C.; Yu, Zicheng

doi:10.1016/j.quascirev.2007.09.016

Cited by 584 publications

(506 citation statements)

References 79 publications

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“…Marked fluctuations in the relative abundance of various pollen taxa are seen at all three sites during this interval, although their timing generally is difficult to relate to fluctuations recognised elsewhere, for example in the Greenland ice core record (Lowe et al, 2008). At liten Čap'pesjav'ri, however, a sustained reduction in relative abundance of pollen of woody taxa and increase in abundance of Artemisia pollen during the last five hundred years of the interval may represent the local expression of the Younger Dryas (GS1, Lowe et al, 2008).…”

Section: Pollen Analysis and Palaeovegetationmentioning

confidence: 83%

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Huntley

Long

Allen

2013

Quaternary Science Reviews

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. (2013) 'Spatio-temporal patterns in late-glacial and Holocene vegetation and climate of Finnmark, northernmost Europe.', Quaternary science reviews., 70 . pp. 158-175. Further information on publisher's website:http://dx.doi.org/10. 1016/j.quascirev.2013.03.006 Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Quaternary Science Reviews. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be re ected in this document. Changes may have been made to this work since it was submitted for publication. A de nitive version was subsequently published in Quaternary Science Reviews, 70, 2013Reviews, 70, , 10.1016Reviews, 70, /j.quascirev.2013 Additional information: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details. Further work on precisely-dated marine sediment cores will be necessary to understand the factors leading to the periodic and longer-term variations in strength of the North Cape Current.

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Section: Pollen Analysis and Palaeovegetationmentioning

confidence: 83%

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Huntley

Long

Allen

2013

Quaternary Science Reviews

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“…Beryllium ratios were determined at the Scottish Universities Environmental Research Centre (SUERC) AMS facility. (Lowe et al, 2008). The mean of the overlapping exposure ages from each of the Sail Mhor, Achiltibuie and Loanan Valley moraines are: 13.5, 13.6 and 13.5 ka respectively.…”

Section: Study Site and Methodsmentioning

confidence: 94%

“…Traditionally, glacial deposits and landforms from the mountains and glens of western Scotland have been ascribed to the Younger Dryas (YD) chronozone (12.9-11.7 ka BP; Greenland Stadial 1 (GS-1) (Lowe et al, 2008)), locally known in Britain as the Loch Lomond Stadial (e.g. Sissons, 1977Sissons, , 1979Ballantyne, 1989Ballantyne, , 2007Bennett and Boulton, 1993;Benn and Lukas, 2006;Golledge, 2007).…”

mentioning

confidence: 99%

Ice caps existed throughout the Lateglacial Interstadial in northern Scotland

Bradwell

Fabel

Stoker

et al. 2008

J Quaternary Science

122

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We constrain, in detail, fluctuations of two former ice caps in NW Scotland with multibeam seabed surveys, geomorphological mapping and cosmogenic 10 Be isotope analyses. We map a continuous sequence of 40 recessional moraines stretching from ~10 km offshore to the Wester Ross mountains. Surface-exposure ages from boulders on moraine ridges in Assynt and the Summer Isles region show that substantial, dynamic, ice caps existed in NW Scotland between 13-14 ka BP. We interpret this as strong evidence that large active glaciers probably survived throughout the Lateglacial Interstadial, and that during the Older Dryas period (c.14 ka BP) ice caps in NW Scotland were thicker and considerably more extensive than in the subsequent Younger Dryas Stadial. By inference, we suggest that Lateglacial ice-cap oscillations in Scotland reflect the complex interplay between changing temperature and precipitation regimes during this climatically unstable period (~15-11 ka BP). words

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“…14.5-12.9 ka; Jouzel et al, 2001) rather than the Younger Dryas cold period in the North Atlantic (ca. 12.9-11.7 ka; 21 Rasmussen et al, 2006;Lowe et al, 2008). An absence of evidence for changes in the IRD or dust records may imply that the advance was either weak or, more probably, a prolonged still stand ( Figure 8K and L).…”

Section: Mis 2 (Ca 29-14 Ka) and The Glgm Period (265-19 Ka)mentioning

confidence: 99%

The timing and cause of glacial advances in the southern mid-latitudes during the last glacial cycle based on a synthesis of exposure ages from Patagonia and New Zealand

Darvill

Bentley

Stokes

et al. 2016

Quaternary Science Reviews

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Synchronisation of palaeoenvironmental events in the North Atlantic region during the Last Termination: a revised protocol recommended by the INTIMATE group

Cited by 584 publications

References 79 publications

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Ice caps existed throughout the Lateglacial Interstadial in northern Scotland

The timing and cause of glacial advances in the southern mid-latitudes during the last glacial cycle based on a synthesis of exposure ages from Patagonia and New Zealand

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