Zobrazeno 1 - 10
of 152
pro vyhledávání: '"TJEERD H. VAN ANDEL"'
Autor:
Tjeerd H. van Andel
In this 1994 revised edition of his award-winning book on the Earth's history, Professor van Andel updates and expands his earlier text, drawing on a wealth of new knowledge that has become available in the last decade. This book examines the major c
Autor:
Tjeerd H. van Andel
Publikováno v:
Landscape and People of the Franchthi Region
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9eb96b2ab311b604728b27794fd0f7d3
https://doi.org/10.2307/j.ctv7vcszh.6
https://doi.org/10.2307/j.ctv7vcszh.6
The location and survival of trees in the coldest stages of the last full-glacial has long been of interest to palaeoecologists, biogeographers, archaeologists and geneticists alike. In particular, where species survived in isolated refugia and the i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::330e7e19122a1bcb5be5c9778cb2beec
https://doi.org/10.1016/j.quascirev.2004.06.002
https://doi.org/10.1016/j.quascirev.2004.06.002
Autor:
Eva Alram-Stern, Gary O. Rollefson, Eva Bauer, Bernhard Weninger, Olaf Jöris, Claudia Kubatzki, Tjeerd H. van Andel, Uwe Danzeglocke, Lee Clare, Henrieta Todorova
Publikováno v:
Quaternary Research. 66:401-420
We explore the hypothesis that the abrupt drainage of Laurentide lakes and associated rapid switch of the North Atlantic thermohaline circulation 8200 yr ago had a catastrophic influence on Neolithic civilisation in large parts of southeastern Europe
Autor:
Tjeerd H. van Andel
Publikováno v:
Antiquity. 79:944-948
Rapid extension of 14C-age dating into the Last Glaciation due to a rising interest in high-resolution climate events is demanding ever greater emphasis on accurate stratigraphic placement of samples relative to events or objects to be dated. This sh
Publikováno v:
Quaternary Research. 57:38-48
The climate of the middle Weichselian Glaciation, Marine Oxygen Isotope Stage 3 (OIS-3), a relatively mild period compared to the glacial maxima of OIS-4 and OIS-2, consisted of long warm interstades punctuated by brief cold excursions that grew cold