3 Records of Quaternary Paleoclimate in the Great Basin

Tuesday, 15 March 2022
8:00 AM - 12:00 PM
CBC-A 108


HYDROCLIMATE RESPONSE OF SPRING ECOSYSTEMS TO A TWO-STAGE YOUNGER DRYAS EVENT IN WESTERN NORTH AMERICA

Paper number: 3-5
Program: Theme Sessions
Time: 9:05 AM – 9:25 AM


Authors


Abstract

The Younger Dryas (YD) climate event is the preeminent example of abrupt climate change in the recent geologic past. Climate conditions during the YD were spatially complex, and high-resolution sediment cores in the North Atlantic, western Europe, and East Asia have revealed it unfolded in two distinct stages, including an initial stable climatic period between ~12.9 and 12.2 ka associated with weakening of the Atlantic Meridional Overturning Circulation (AMOC) followed by unstable conditions until 11.7 ka as the AMOC recovered. Despite decades of investigations, unequivocal evidence of this stepped phenomenon has not been identified in western North America. Here we present new hydroclimate data from paleospring deposits from the Rogers Basin in northern Death Valley National Park (California, USA) that document high groundwater levels persisted in this part of the valley during the entirety of the YD event and demonstrate that two-stage partitioning of the YD event occurred in temporal synchroneity with proxy records elsewhere in the Northern Hemisphere. Stable and long-lived spring ecosystems prevailed in the Rogers Basin between ~13.0 and 12.2 ka, and were immediately replaced by alternating wet and dry environments until ~11.8 ka. This hydrologic record provides robust evidence of the two-stage nature of the YD event, firmly establishes that this intra-YD climate transition extended into western North America, and shows that even short-lived changes in the AMOC can have profound consequences for ecosystems worldwide. Further, these results provide valuable data for climate modeling and other studies aimed at reconstructing hydroclimate conditions in western North America during the late Pleistocene.

Geological Society of America Abstracts with Programs. Vol. 54, No. 2

doi: 10.1130/abs/2022CD-374025

© Copyright 2022 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.