An annual-resolution stable isotope record from Swiss subfossil pine trees growing in the late Glacial

0536274 - ÚVGZ 2021 RIV GB eng J - Journal Article
Pauly, M. - Helle, G. - Büntgen, Ulf - Wacker, L. - Treydte, K. - Reinig, F. - Turney, C. - Nievergelt, D. - Kromer, B. - Friedrich, M. - Sookdeo, A. - Heinrich, I. - Riedel, F. - Balting, D. - Brauer, A.
An annual-resolution stable isotope record from Swiss subfossil pine trees growing in the late Glacial.
Quaternary Science Reviews. Roč. 247, NOV (2020), č. článku 106550. ISSN 0277-3791. E-ISSN 1873-457X
R&D Projects: GA ČR(CZ) GA17-22102S
Institutional support: RVO:86652079
Keywords : 2 minor oscillations * younger dryas * oxygen isotopes * atmospheric circulation * radiocarbon calibration * gerzensee switzerland * ring chronologies * carbon-isotope * central-europe * climate-change * Tree-ring cellulose * delta O-13 * delta O-18 * Late glacial * Switzerland * Climate
OECD category: Physical geography
Impact factor: 4.112, year: 2020
Method of publishing: Limited access
https://www.sciencedirect.com/science/article/pii/S0277379120305126?via%3Dihub

Previous studies have suggested that the Late Glacial period (LG,14 600-11 700 cal BP) was characterised by abrupt and extreme climate variability over the European sector of the North Atlantic. The limited number of precisely dated, high-resolution proxy records, however, restricts our understanding of climate dynamics through the LG. Here, we present the first annually-resolved tree-cellulose stable oxygen and carbon isotope chronology (delta O-18(tree), delta C-13(tree)) covering the LG between similar to 14 050 and 12 795 cal BP, generated from a Swiss pine trees (P. sylvestris, 27 trees, 1255 years).
Permanent Link: http://hdl.handle.net/11104/0314142