Reconstructing distribution of the Eastern Rock Nuthatch during the Last Glacial Maximum and Last Interglacial
نویسندگان
چکیده
منابع مشابه
The Last Glacial Maximum.
We used 5704 14C, 10Be, and 3He ages that span the interval from 10,000 to 50,000 years ago (10 to 50 ka) to constrain the timing of the Last Glacial Maximum (LGM) in terms of global ice-sheet and mountain-glacier extent. Growth of the ice sheets to their maximum positions occurred between 33.0 and 26.5 ka in response to climate forcing from decreases in northern summer insolation, tropical Pac...
متن کاملSimulating last interglacial and glacial inception
Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion EGU Abstract The Planet Simulator was used to perform equilibrium simulations of the Eemian inter-glacial at 125 kyBP and the glacial inception at 115 kyBP. Additio...
متن کاملThe tropical lapse rate steepened during the Last Glacial Maximum
The gradient of air temperature with elevation (the temperature lapse rate) in the tropics is predicted to become less steep during the coming century as surface temperature rises, enhancing the threat of warming in high-mountain environments. However, the sensitivity of the lapse rate to climate change is uncertain because of poor constraints on high-elevation temperature during past climate s...
متن کاملLast glacial-interglacial productivity and associated changes in the eastern Arabian Sea
Article history: Received 8 February 2016 Received in revised form 5 July 2016 Accepted 9 July 2016 Available online xxxx Wereconstruct paleo-productivity and bottomwater oxygenation changes during thepast 32 ka, from the southeastern Arabian Sea, using absolute abundance of planktic foraminifera, relative abundance of Globigerina bulloides, angular asymmetrical benthic foraminifera (AABF), mea...
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ژورنال
عنوان ژورنال: Avian Biology Research
سال: 2019
ISSN: 1758-1559,1758-1567
DOI: 10.1177/1758155919874537