authors write “Owingtothelowcavetemperaturekineticisotopeeffectsareminimal (Mangini et al., 2005; Vollweiler et al., 2006). The short-term variations in COMNISPA II are in response to temperature, whereas for the late Holocene (the last 2 ka) Mangini et al. (2005) provided a transfer function between stalagmite δ18O values and air temperature. They showed that for Spannagel cave higher δ18O values characterize a colder climate and vice versa”

Variable name changed from age to depth during update from DKs csv files.

Variable name changed from age to thickness during update from DKs csv files.

Variable name changed from age to age error during update from DKs csv files.

Variable name changed from age to 238U_content during update from DKs csv files.

Variable name changed from age to 238U_uncertainty during update from DKs csv files.

Variable name changed from age to 232Th_content during update from DKs csv files.

Variable name changed from age to 232Th_uncertainty during update from DKs csv files.

Variable name changed from age to 230Th_content during update from DKs csv files.

Fohlmeister, Jens; Vollweiler, Nicole; Sp̦tl, Christoph; Mangini, Augusto

COMNISPA II: Update of a mid-European isotope climate record, 11 ka to present

Holocene vegetation, climate, and fire history of the Hudson Highlands, southeastern New York, USA

North America>United States Of America>New York

Jung-Hyun Kim, Norel Rimbu, Stephan J. Lorenz, Gerrit Lohmann, Seung-IlNam, Stefan Schouten, Carsten Ruhlemann, Ralph R. Schneider (2004): North Pacific and North Atlantic sea-surface temperature variability during the Holocene. Quaternary Science Reviews, 23, 2141-2154, doi:10.1016/j.quascirev.2004.08.010

Yoo, Dong G., Seong P. Kim, Tae S. Chang, Gee S. Kong, Nyeon K. Kang, Yi K. Kwon, Seung L. Nam, and Soo C. Park (2014): Late Quaternary inner shelf deposits in response to late Pleistocene⁈olocene sea level changes: Nakdong River, SE Korea. Quaternary International, 344, 156-169, doi:10.1016/j.quaint.2014.02.004