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Foraminiferal changes and geochemical profiles across the Cenomanian/Turonian boundary in central and south‐east Poland
Author(s) -
Peryt Danuta,
Wyrwicka Krystyna,
Orth Charles,
Attrep Moses,
Quintana Leonard R.
Publication year - 1994
Publication title -
terra nova
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.353
H-Index - 89
eISSN - 1365-3121
pISSN - 0954-4879
DOI - 10.1111/j.1365-3121.1994.tb00649.x
Subject(s) - cenomanian , geology , facies , paleontology , isotopes of carbon , stable isotope ratio , carbonate , anoxic waters , mineralogy , cretaceous , geochemistry , total organic carbon , oceanography , chemistry , structural basin , environmental chemistry , physics , quantum mechanics , organic chemistry
Two sections of the Upper Cenomanian and Lower Turonian in central and south‐east Poland were investigated for foraminifers, CaCO 3 content, carbon content insoluble in HCl (C org ) and in the carbonates (C carb ), carbon and oxygen isotopic composition of bulk‐rock carbonates and elemental abundances. The Cenomanian/Turonian boundary interval is characterized by the appearance of more marly facies, a δ 13 C and δ 18 O stable isotope anomaly, a considerable increase in C org content and decrease in C carb content and substantial changes in the foraminiferal assemblages. A major carbon stable isotope excursion with a shift of +2 (PDB) occurs in the lowermost Whiteinella archaeocretacea Zone. The late Cenomanian δ 13 C anomaly is associated with heavy δ 18 O values. The peak value of δ 13 C corresponds to the minima in P/B ratio and in diversity of foraminiferal assemblages. A late Cenomanian anoxic event is thought to be responsible for changes in foraminiferal assemblages. However, elemental abundance analyses do not show changes in the concentrations of trace elements. This may be explained by the long distance between studied area and a source of enrichment which was probably located in the western hemisphere.