Oldest Dryas

Dryas octopetala is the indicator species for the period

The Oldest Dryas[a] is a biostratigraphic subdivision layer corresponding to a relatively abrupt climatic cooling event, or stadial, which occurred during the last glacial retreat.[1][2] The time period to which the layer corresponds is poorly defined and varies between regions,[1] but it is generally dated as starting at 18.5–17 thousand years (ka) before present (BP) and ending 15–14 ka BP.[3][4][5][6][7] As with the Younger and Older Dryas events, the stratigraphic layer is marked by abundance of the pollen and other remains of Dryas octopetala, an indicator species that colonizes arctic-alpine regions. The termination of the Oldest Dryas is marked by an abrupt oxygen isotope excursion, which has been observed at many sites in the Alps that correspond to this interval of time.[8]

In the Alps, the Oldest Dryas corresponds to the Gschnitz stadial of the Würm glaciation. The term was originally defined specifically for terrestrial records in the region of Scandinavia, but has come to be used both for ice core stratigraphy in areas across the world, and to refer to the time period itself and its associated temporary reversal of the glacial retreat.[1]

In the Iberian Peninsula, the glaciers of the Pyrenees, Sierra Nevada, Central Range, and Northwestern Mountains, which had almost entirely disappeared by 17,500 BP, began to advance once again. Between 16,800 and 16,500 BP, these glaciers abruptly advanced into montane valleys and deposited moraines near the moraines formed during the Last Glacial Maximum. These glaciers then began to oscillate between advance and retreat until a final glacial advance at 15,500 BP. A thousand years later, following a general glacial retreat, these alpine glaciers were relegated to cirques.[9]

The edge of the ice in Greenland


Cite error: There are <ref group=lower-alpha> tags or {{efn}} templates on this page, but the references will not show without a {{reflist|group=lower-alpha}} template or {{notelist}} template (see the help page).

  1. ^ a b c Rasmussen, Sune O.; Bigler, Matthias; Blockley, Simon P.; Blunier, Thomas; Buchardt, Susanne L.; Clausen, Henrik B.; Cvijanovic, Ivana; Dahl-Jensen, Dorthe; Johnsen, Sigfus J.; Fischer, Hubertus; Gkinis, Vasileios; Guillevic, Myriam; Hoek, Wim Z.; Lowe, J. John; Pedro, Joel B.; Popp, Trevor; Seierstad, Inger K.; Steffensen, Jørgen Peder; Svensson, Anders M.; Vallelonga, Paul; Vinther, Bo M.; Walker, Mike J.C.; Wheatley, Joe J.; Winstrup, Mai (December 2014). "A Stratigraphic Framework for Abrupt Climatic Changes during the Last Glacial Period Based on Three Synchronized Greenland Ice-core Records: Refining and Extending the INTIMATE Event Stratigraphy". Quaternary Science Reviews. 106. Amsterdam: Elsevier: 14–28. Bibcode:2014QSRv..106...14R. doi:10.1016/j.quascirev.2014.09.007. hdl:2160/30436.
  2. ^ Hoek, Wim (2009). "Bølling-Allerød Interstadial". In Gornitz, Vivien (ed.). Encyclopedia of Paleoclimatology and Ancient Environments. Dordrecht: Springer. ISBN 978-1-4020-4551-6. Retrieved 15 January 2021.
  3. ^ Carlson, Anders E.; Winsor, Kelsey (26 August 2012). "Northern Hemisphere Ice-sheet Responses to Past Climate Warming" (PDF). Nature Geoscience. 5 (9). London: Nature Portfolio: 607–613. Bibcode:2012NatGe...5..607C. doi:10.1038/NGEO1528. Archived from the original (PDF) on 30 August 2021. Retrieved 5 July 2019.
  4. ^ Clark, P. U.; Shakun, J. D.; Baker, P. A.; Bartlein, P. J.; Brewer, S.; Brook, E.; Carlson, A. E.; Cheng, H.; Kaufman, D. S.; Liu, Z.; Marchitto, T. M.; Mix, A. C.; Morrill, C.; Otto-Bliesner, B. L.; Pahnke, K.; Russell, J. M.; Whitlock, C.; Adkins, J. F.; Blois, J. L.; Clark, J.; Colman, S. M.; Curry, W. B.; Flower, B. P.; He, F.; Johnson, T. C.; Lynch-Stieglitz, J.; Markgraf, V.; McManus, J.; Mitrovica, J. X.; Moreno, P. I.; Williams, J. W. (13 February 2012). "Global Climate Evolution during the Last Deglaciation". Proceedings of the National Academy of Sciences. 109 (19). Washington: National Academy of Sciences: E1134–E1142. doi:10.1073/pnas.1116619109. PMC 3358890. PMID 22331892.
  5. ^ Roberts, Neil (2014). The Holocene: An Environmental History (3rd ed.). Oxford: John Wiley & Sons. p. 98. ISBN 978-1-4051-5521-2.
  6. ^ Shakun, Jeremy D.; Carlson, Anders E. (July 2010). "A Global Perspective on Last Glacial Maximum to Holocene Climate Change" (PDF). Quaternary Science Reviews. 29 (15–16). Amsterdam: Elsevier: 1801–1816. Bibcode:2010QSRv...29.1801S. doi:10.1016/j.quascirev.2010.03.016. Archived from the original (PDF) on 24 December 2015. Retrieved 5 July 2019.
  7. ^ Zheng, Yanhong; Pancost, Richard D.; Liu, Xiaodong; Wang, Zhangzhang; Naafs, B.D.A.; Xie, Xiaoxun; Liu, Zhao; Yu, Xuefeng; Yang, Huan (2 October 2017). "Atmospheric Connections with the North Atlantic Enhanced the Deglacial Warming in Northeast China". Geology. 45 (11). Boulder: Geological Society of America: 1031–1034. Bibcode:2017Geo....45.1031Z. doi:10.1130/G39401.1.
  8. ^ Eicher, U.; Siegenthaler, U.; Wegmüller, S. (20 January 2017). "Pollen and Oxygen Isotope Analyses on Late- and Post-Glacial Sediments of the Tourbière de Chirens (Dauphiné, France)". Quaternary Research. 15 (2): 160–170. doi:10.1016/0033-5894(81)90102-2. S2CID 129570510. Retrieved 14 April 2023.
  9. ^ Palacios, David; De Andrés, Nuria; Gómez-Ortiz, Antonio; García-Ruiz, José M. (18 January 2016). "Evidence of glacial activity during the Oldest Dryas in the mountains of Spain". Geological Society, London, Special Publications. 433: 87–110. doi:10.1144/sp433.10. S2CID 131340591. Retrieved 15 April 2023.