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Reconciliation of the Devils Hole climate record with orbital forcing

  • Gina E. Moseley
  • , R. Lawrence Edwards
  • , Kathleen A. Wendt
  • , Hai Cheng
  • , Yuri Dublyansky
  • , Yanbin Lu
  • , Ronny Boch
  • , Christoph Spötl
  • University of Innsbruck
  • University of Minnesota Twin Cities
  • Graz University of Technology

Research output: Contribution to journalArticlepeer-review

64 Scopus citations

Abstract

The driving force behind Quaternary glacial-interglacial cycles and much associated climate change is widely considered to be orbital forcing. However, previous versions of the iconic Devils Hole (Nevada) subaqueous calcite record exhibit shifts to interglacial values ∼10,000 years before orbitally forced ice age terminations, and interglacial durations ∼10,000 years longer than other estimates. Our measurements from Devils Hole 2 replicate virtually all aspects of the past 204,000 years of earlier records, except for the timing during terminations, and they lower the age of the record near Termination II by ∼8000 years, removing both ∼10,000-year anomalies. The shift to interglacial values now broadly coincides with the rise in boreal summer insolation, the marine termination, and the rise in atmospheric CO2, which is consistent with mechanisms ultimately tied to orbital forcing.

Original languageEnglish
Pages (from-to)165-168
Number of pages4
JournalScience
Volume351
Issue number6269
DOIs
StatePublished - 8 Jan 2016

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 14 - Life Below Water
    SDG 14 Life Below Water

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