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BARDET, N., CAPPETTA, H., PEREDA SUBERBIOLA, X., MOUTY, M., AL MALEH, A. K., AHMAD, A. M., KHRATA, O., GANNOUM, N. (2000) The marine vertebrate faunas from the Late Cretaceous phosphates of Syria. Geological Magazine, 137 (3) 269-290 doi:10.1017/s0016756800003988

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Reference TypeJournal (article/letter/editorial)
TitleThe marine vertebrate faunas from the Late Cretaceous phosphates of Syria
JournalGeological Magazine
AuthorsBARDET, N.Author
CAPPETTA, H.Author
PEREDA SUBERBIOLA, X.Author
MOUTY, M.Author
AL MALEH, A. K.Author
AHMAD, A. M.Author
KHRATA, O.Author
GANNOUM, N.Author
Year2000 (May)Volume137
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800003988Search in ResearchGate
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Mindat Ref. ID258388Long-form Identifiermindat:1:5:258388:8
GUID0
Full ReferenceBARDET, N., CAPPETTA, H., PEREDA SUBERBIOLA, X., MOUTY, M., AL MALEH, A. K., AHMAD, A. M., KHRATA, O., GANNOUM, N. (2000) The marine vertebrate faunas from the Late Cretaceous phosphates of Syria. Geological Magazine, 137 (3) 269-290 doi:10.1017/s0016756800003988
Plain TextBARDET, N., CAPPETTA, H., PEREDA SUBERBIOLA, X., MOUTY, M., AL MALEH, A. K., AHMAD, A. M., KHRATA, O., GANNOUM, N. (2000) The marine vertebrate faunas from the Late Cretaceous phosphates of Syria. Geological Magazine, 137 (3) 269-290 doi:10.1017/s0016756800003988
In(2000, May) Geological Magazine Vol. 137 (3) Cambridge University Press (CUP)
Abstract/NotesMarine vertebrate faunas from the latest Cretaceous phosphates of the Palmyrides Chain of
Syria are described for the first time. Recent fieldwork in the phosphatic deposits of the Palmyra area
(mines of Charquieh and Khneifiss, outcrops of Bardeh, Soukkari and Soukhneh) have yielded a rich
and diversified assemblage of marine vertebrates, including more than 50 species of chondrichthyes,
osteichthyes, squamates, chelonians, plesiosaurians and crocodilians. Selachians are the most abundant
and diverse component of the faunas and are represented by at least 34 species of both sharks
and rays. Actinopterygians include representatives of six families, the most common being the
enchodontids. Squamates are known by six mosasaurid species and an indeterminate varanoid.
Chelonians are represented by at least two bothremydids and two chelonioids. Finally, elasmosaurid
plesiosaurs and indeterminate crocodilians are also present in the fossil assemblages. The difference in
faunal composition observed between the sites is interpreted as being due to palaeoecological preferences
related to the Hamad Uplift palaeostructure. The marine vertebrate faunas of Syria show close
affinities with those of the latest Cretaceous phosphatic deposits of North Africa and the Middle East
and are typical of the southern Tethyan realm. From a biostratigraphical point of view, the selachians
are the only suitable material to provide elements of an answer to the long debated question of the age
of the Syrian Senonian phosphates. They suggest an Early Maastrichtian age for most of the phosphates
of the Palmyrides Chain.


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