FN Archimer Export Format
PT J
TI The coastal archives of the last 15 ka in the Atlantic-Mediterranean Spanish linkage area: Sea level and climate changes
BT 
AF ZAZO, C.
   DABRIO, C. J.
   GOY, J. L.
   LARIO, J.
   CABERO, A.
   SILVA, P.G.
   BARDAJI, T.
   MERCIER, N.
   BORJA, F.
   ROQUERO, E.
AS 1:1;2:2;3:3;4:4;5:1;6:3;7:5;8:6;9:7;10:8;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;
C1 CSIC, Museo Nacl Ciencias Nat, Dept Geol, E-28006 Madrid, Spain.
   Univ Complutense, Inst Geol Econ, Dept Estratig, E-28040 Madrid, Spain.
   Univ Salamanca, Dept Geol, E-37008 Salamanca, Spain.
   Univ Nacl Educ Distancia, Fac Ciencias, Dept Ciencias Analit, E-28040 Madrid, Spain.
   Univ Alcala de Henares, Dept Geol, Alcala De Henares 28871, Spain.
   CEA, CNRS, Lab Sci Climat Environm, F-91198 Gif Sur Yvette, France.
   Univ Huelva, Fac Humanidades, Area Geog Fis, Huelva 21007, Spain.
   Univ Politecn Madrid, ETSI, Dept Edafol, E-28040 Madrid, Spain.
C2 CSIC, SPAIN
   UNIV COMPLUTENSE MADRID, SPAIN
   UNIV SALAMANCA, SPAIN
   UNIV NACL EDUC DISTANCIA, SPAIN
   UNIV ALCALA DE HENARES, SPAIN
   CEA, FRANCE
   UNIV HUELVA, SPAIN
   UNIV POLITECN MADRID, SPAIN
IF 1.482
TC 93
UR https://archimer.ifremer.fr/doc/00237/34864/82769.pdf
LA English
DT Article
CR IMAGES 1-MD101
BO Marion Dufresne
AB Sea level and climate changes archived in various coastal environments during the last part of the last glacial and present interglacial periods are investigated by interpolating available geomorphology, sedimentology, palacontology and geochronology data. The coastal response to these changes depended on the environment and geographic location. Changes of sea level during the rising, transgressive phase are well recorded in the sedimentary filling of the estuaries, whereas during the phase of highstand they are best recorded in beach-barrier environments. The postglacial rise of sea level took place in two phases: a rapid rise until 6500 cal BP, and a second phase of near stability with minor oscillations of metric magnitude. Regarding climate changes, there is no record of changing temperatures in the coastal zones of southern Spain, although there is in precipitation and wind intensity/velocity. After 7-5cal ka BP, the general climatic trend towards aridity was punctuated by several short-lived (centennial) episodes of increased aridity that occurred with a millennial cycle, often coincident with Bond cool events and, in some cases, with decreases of sea surface temperatures. The absence of human intervention in vegetation composition until 2000 BP suggests that most environmental coastal shifts were climatically driven.
PY 2008
PD APR
SO Quaternary International
SN 1040-6182
PU Pergamon-elsevier Science Ltd
VL 181
IS 1
UT 000256411700008
BP 72
EP 87
DI 10.1016/j.quaint.2007.05.021
ID 34864
ER

EF