| Literature DB >> 33602851 |
Alan Cooper1,2, Chris S M Turney3, Jonathan Palmer4, Alan Hogg5, Matt McGlone6, Janet Wilmshurst6,7, Andrew M Lorrey8, Timothy J Heaton9, James M Russell10, Ken McCracken11, Julien G Anet12, Eugene Rozanov13,14,15, Marina Friedel13, Ivo Suter16, Thomas Peter13, Raimund Muscheler17, Florian Adolphi18, Anthony Dosseto19, J Tyler Faith20, Pavla Fenwick21, Christopher J Fogwill22, Konrad Hughen23, Mathew Lipson24, Jiabo Liu25, Norbert Nowaczyk26, Eleanor Rainsley22, Christopher Bronk Ramsey27, Paolo Sebastianelli28, Yassine Souilmi29, Janelle Stevenson30,31, Zoë Thomas4, Raymond Tobler29, Roland Zech32.
Abstract
Geological archives record multiple reversals of Earth's magnetic poles, but the global impacts of these events, if any, remain unclear. Uncertain radiocarbon calibration has limited investigation of the potential effects of the last major magnetic inversion, known as the Laschamps Excursion [41 to 42 thousand years ago (ka)]. We use ancient New Zealand kauri trees (Agathis australis) to develop a detailed record of atmospheric radiocarbon levels across the Laschamps Excursion. We precisely characterize the geomagnetic reversal and perform global chemistry-climate modeling and detailed radiocarbon dating of paleoenvironmental records to investigate impacts. We find that geomagnetic field minima ~42 ka, in combination with Grand Solar Minima, caused substantial changes in atmospheric ozone concentration and circulation, driving synchronous global climate shifts that caused major environmental changes, extinction events, and transformations in the archaeological record.Entities:
Year: 2021 PMID: 33602851 DOI: 10.1126/science.abb8677
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728