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The Weichselian Late‐glacial in southwestern Europe (Iberian Peninsula, Pyrenees, Massif Central, northern Apennines)
Author(s) -
de Beaulieu J. L.,
Andrieu V.,
Ponel P.,
Reille M.,
Lowe J. J.
Publication year - 1994
Publication title -
journal of quaternary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.142
H-Index - 94
eISSN - 1099-1417
pISSN - 0267-8179
DOI - 10.1002/jqs.3390090203
Subject(s) - younger dryas , massif , glacial period , geology , peninsula , radiocarbon dating , holocene , physical geography , allerød oscillation , preboreal , paleontology , archaeology , geography
This paper presents a summary of Late‐glacial environmental changes in southwestern Europe (lberian Peninsula, Pyrenees, Massif Central and the northern Apennines). The emphasis is on palaeoclimatic interpretations inferred from key sites in the region from which the most detailed records are available and which have been radiocarbon dated. The earliest evidence for climatic improvement following the end of the last glacial stage is dated to ca. 15 ka BP and is found at a few sites only. By 13 ka BP, a more widespread and marked climatic improvement is evident, although it is difficult to be precise in the timing and magnitude of the event. There are significant variations in detail between the Late‐glacial records, but evidence for a significant cooling correlated with the Younger Dryas event is widespread throughout the region. Just two sites in the region provide evidence for an earlier, less emphatic phase of climatic cooling, which is tentatively equated with the ‘Older Dryas’ of continental northern Europe. Dry conditions appear to have predominated throughout the region in the later part of the Younger Dryas and the early Holocene.