TY - JOUR
T1 - Acid-resistant Cretaceous thecamoebian tests from the Arabian Peninsula: a suggestion for study of agglutinated rhizopods in palynological slides
AU - Kumar, Arun
PY - 2011
Y1 - 2011
N2 - Rare specimens of Centropyxis aculeata (Ehrenberg, 1832), cf. Difflugia oblonga (Ehrenberg, 1832), Amphitrema flavum (Archer, 1869) and an unidentified spherical form (similar to a protozoan 'cyst' in van Hengstum et al., 2007) were observed in the palynological preparations of cutting samples from a drill-hole in southern Saudi Arabia. These thecamoebians were found in Cretaceous formations in association with typical Cretaceous spore, pollen and dinoflagellate cysts. Since the youngest rock formation in this drill-hole is of Cretaceous age, contamination due to caving from post-Cretaceous sediments is thus ruled out. Although the oldest record of thecamoebians comes from Neoproterozoic strata, their pre-Holocene occurrences are rare and patchy. Since many thecamoebian tests are autogenous and are made of acid-resistant proteinaceous material, they occur in the palynological preparations of fossil sediments. It is suggested that careful observation and search for thecamoebians in paly
AB - Rare specimens of Centropyxis aculeata (Ehrenberg, 1832), cf. Difflugia oblonga (Ehrenberg, 1832), Amphitrema flavum (Archer, 1869) and an unidentified spherical form (similar to a protozoan 'cyst' in van Hengstum et al., 2007) were observed in the palynological preparations of cutting samples from a drill-hole in southern Saudi Arabia. These thecamoebians were found in Cretaceous formations in association with typical Cretaceous spore, pollen and dinoflagellate cysts. Since the youngest rock formation in this drill-hole is of Cretaceous age, contamination due to caving from post-Cretaceous sediments is thus ruled out. Although the oldest record of thecamoebians comes from Neoproterozoic strata, their pre-Holocene occurrences are rare and patchy. Since many thecamoebian tests are autogenous and are made of acid-resistant proteinaceous material, they occur in the palynological preparations of fossil sediments. It is suggested that careful observation and search for thecamoebians in paly
M3 - Article
SN - 0262-821X
JO - Journal of Micropalaeontology
JF - Journal of Micropalaeontology
ER -