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Journal article

Controls on the southwest USA hydroclimate over the last six glacial-interglacial cycles

Abstract:

The Great Basin in the southwest United States experienced major hydroclimate shifts throughout the Quaternary. Understanding the drivers behind these past changes has become increasingly important for improving future climate projections. Here, we present an absolute-dated δ18O and δ13C record from Devils Hole cave 2 (southern Nevada) that reveals climate and environmental changes in the southern Great Basin over the last 580,000 years. Water isotope-enabled Earth system simulations and phasing analysis show that temperature-related mechanisms are a primary driver of δ18O variability, with additional drivers stemming from processes linked to North American ice sheets. Vegetation density in the highlands of southern Nevada is primarily forced by Northern Hemisphere summer intensity. A rapid decline in primary productivity occurs during warm interglacial periods when local groundwater recharge declines to <50% above modern. Our study sheds new light on the relationship between temperature, moisture balance, and vegetation over the last six glacial-interglacial cycles.

Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1038/s41467-025-64963-1

Authors


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Role:
Author
ORCID:
0000-0001-8905-5013
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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
ORCID:
0000-0001-7181-2370
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Role:
Author
ORCID:
0000-0002-2227-1747
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Role:
Author
ORCID:
0000-0002-3391-1463


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Funder identifier:
https://ror.org/021nxhr62
Grant:
2102944


Publisher:
Springer Nature
Journal:
Nature Communications More from this journal
Volume:
16
Issue:
1
Article number:
10007
Publication date:
2025-11-14
Acceptance date:
2025-10-01
DOI:
EISSN:
2041-1723


Language:
English
Keywords:
Pubs id:
2327057
UUID:
uuid_4b897f5a-31c2-47be-9244-9004c55359cf
Local pid:
pubs:2327057
Deposit date:
2025-11-14

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