Palaeoenvironmental conditions preceding the Messinian Salinity Crisis: A case study from Gavdos Island

Επιστημονική δημοσίευση - Άρθρο Περιοδικού uoadl:3017509 38 Αναγνώσεις

Μονάδα:
Ερευνητικό υλικό ΕΚΠΑ
Τίτλος:
Palaeoenvironmental conditions preceding the Messinian Salinity Crisis: A case study from Gavdos Island
Γλώσσες Τεκμηρίου:
Αγγλικά
Περίληψη:
The Messinian pre-evaporitic sedimentary succession of Gavdos Island (Metochia section) is a nearly uninterrupted succession of marine sediments, dominated by finely laminated diatomaceous marls, which are cyclically alternating with clayey diatomites and white diatomites. The qualitative and quantitative analysis of the planktonic foraminiferal fauna allowed the recognition of nine bioevents, which have been astronomically dated for the Mediterranean. The base of the diatomitic succession in Gavdos Island is dated at 6.722 Ma and the top at 6.015 Ma. The studied section contains benthic foraminiferal genera characteristic of an outer shelf to slope environment. The qualitative and quantitative analysis of this microfauna revealed three benthic foraminiferal fossil assemblages and the occurrence of allochthonous species transported into the bathyal environment by current activity. The cyclical pattern of the benthic foraminifera assemblages indicates that the studied sediments have been affected by repeated episodes of basin restriction characterized by low diversity benthic foraminifera populations, and a limited planktonic foraminifer association typified by shallow, surface-dwelling forms. This restriction was partly due to Antarctic cooling, which produced palaeo-Mediterranean sea-level oscillations during the Early Messinian, as a prelude to closure of the Atlantic connections. The relative impact of climatic versus tectonic control on sedimentation patterns within this basin is discussed. © 2007 Elsevier Masson SAS. All rights reserved.
Έτος δημοσίευσης:
2007
Συγγραφείς:
Drinia, H.
Antonarakou, A.
Tsaparas, N.
Kontakiotis, G.
Περιοδικό:
GEOBIOS
Εκδότης:
Elsevier Masson SAS
Τόμος:
40
Αριθμός / τεύχος:
3
Σελίδες:
251-265
Λέξεις-κλειδιά:
benthic foraminifera; biostratigraphy; diatomite; environmental conditions; extreme event; fossil assemblage; Messinian; paleoenvironment; planktonic foraminifera; salinity; sea level change; species occurrence; succession, Canea; Crete; Eurasia; Europe; Gavdos; Greece; Southern Europe, Foraminifera
Επίσημο URL (Εκδότης):
DOI:
10.1016/j.geobios.2007.02.003
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