TY - JOUR
T1 - Aspidiscus cristatus (lamarck) from the cenomanian sediments of wadi quseib, east sinai, Egypt
AU - Pandey, D. K.
AU - Fürsich, Franz T.
AU - Gameil, M.
AU - Ayoub-Hannaa, W. S.
PY - 2011/6/30
Y1 - 2011/6/30
N2 - Aspidiscus cristatus (Lamarck) has been described and illustrated from three coral-bearing horizons of the Cenomanian sedimentary succession of Wadi Quseib, East Sinai, Egypt. The new specimens show well-preserved internal microarchitectures, which corroborate its assignment to family Latomeandridae Alloiteau, 1952. The stratigraphic range of Aspidiscus cristatus suggests that it can be used as index for the Middle to early Late Cenomanian. Based on the morphology of Aspidiscus cristatus and its consistent record, it is suggested here that the coral had a narrow facies range, being adapted to a free mode of life on soft, marly to argillaceous substrate, in low-energy environments subjected to high rates of sedimentation.
AB - Aspidiscus cristatus (Lamarck) has been described and illustrated from three coral-bearing horizons of the Cenomanian sedimentary succession of Wadi Quseib, East Sinai, Egypt. The new specimens show well-preserved internal microarchitectures, which corroborate its assignment to family Latomeandridae Alloiteau, 1952. The stratigraphic range of Aspidiscus cristatus suggests that it can be used as index for the Middle to early Late Cenomanian. Based on the morphology of Aspidiscus cristatus and its consistent record, it is suggested here that the coral had a narrow facies range, being adapted to a free mode of life on soft, marly to argillaceous substrate, in low-energy environments subjected to high rates of sedimentation.
UR - http://www.scopus.com/inward/record.url?scp=84861535208&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84861535208&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:84861535208
SN - 0552-9360
VL - 56
SP - 29
EP - 37
JO - Journal of the Palaeontological Society of India
JF - Journal of the Palaeontological Society of India
IS - 1
ER -