Calcareous nannofossil biostratigraphy and petrological analysis of the pre-evaporitic diatomaceous sediments from Gavdos Island, southern Greece

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Calcareous nannofossil biostratigraphy and petrological analysis of the pre-evaporitic diatomaceous sediments from Gavdos Island, southern Greece (EN)

Tsaparas, N (EN)
Stamatakis, M (EN)
Dermitzakis, MD (EN)
Triantaphyllou, MV (EN)

journalArticle (EN)

2014-03-01T01:48:50Z
1999 (EN)


The main goal of this study is the biostratigraphical and petrological analysis of the Upper Miocene diatomaceous sediments of Gavdos Island, Greece. The studied sequence is dominated by finely laminated diatomaceous sediments which are cyclically alternating with marlstone and white limestone beds. The biostratigraphical analysis based on calcareous nannofossils achieved the correlation of the diatomaceous marine sediments of Gavdos Island with Zone CN 9b (OKADA & BUKRY 1980) and with the upper part of the Zone NN 11 (MARTINI 1971) or with the C. leptoporus Zone (THEODORIDIS 1984), which chronostratigraphically indicate a Messinian age. The presence of small Gephyrocapsa spp. (forms which generally appear in the Lower Pliocene) in the studied sediments is reported for the first time from the Greek area. Additionally the non-birefringent ceratoliths are well represented including also the species Amaurolithus tricorniculatus. Moreover the extremely rare occurrence of birefringent ceratoliths has been shown. On the other hand the applied petrological studies demonstrate that the diatom layers are rich in amorphous silica (opal - A) and calcite characteristic of an embryonic silica diagenesis, whereas huntite, elastic quartz and feldspars are also present. (EN)

Paleontology (EN)

MIOCENE (EN)
DIAGENESIS (EN)

NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-MONATSHEFTE (EN)

Αγγλική γλώσσα

E SCHWEIZERBARTSCHE VERLAGS (EN)




*Η εύρυθμη και αδιάλειπτη λειτουργία των διαδικτυακών διευθύνσεων των συλλογών (ψηφιακό αρχείο, καρτέλα τεκμηρίου στο αποθετήριο) είναι αποκλειστική ευθύνη των αντίστοιχων Φορέων περιεχομένου.