(Table 1) Oxygen and carbon isotope data of bulk carbonate and foraminiferal species across the Cretaceous/Tertiary boundary at ODP Site 119-738

• Main Authors: Barrera, Enriqueta C, Keller, Gerta
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 1994
• Subjects: DEPTH, sediment/rock; Sample code/label; Planktic foraminifera zone; δ18O, carbonate; δ13C, carbonate; Gavelinella beccariiformis, δ18O; Gavelinella beccariiformis, δ13C; Alabamina creta, δ18O; Alabamina creta, δ13C; Chiloguembelina waiparaensis, δ18O; Chiloguembelina waiparaensis, δ13C; Neoeponides lunata, δ18O; Neoeponides lunata, δ13C; Heterohelix globulosa, δ18O; Heterohelix globulosa, δ13C; Subbotina pseudobulloides, δ18O; Subbotina pseudobulloides, δ13C; Composite Core; DSDP/ODP/IODP sample designation; Mass spectrometer Finnigan MAT 251; Leg119; Joides Resolution; Ocean Drilling Program ODP; Antarctic; Indian; The Antarctic; Antarc*
• Online Access: https://dx.doi.org/10.1594/pangaea.717726; https://doi.pangaea.de/10.1594/PANGAEA.717726

In low and middle latitudes, the Cretaceous/Tertiary boundary is marked by a sudden and pronounced decrease in d13C values of near-surface-water carbonates and a reduction in the surface-to-bottom d13C gradient. These isotopic data have been interpreted as evidence of a decline in surface-water productivity that was responsible for the extinction of many planktic foraminiferal species and other marine organisms at or near the K/T boundary. We present planktic and benthic foraminiferal isotopic data from two almost biostratigraphically complete sections at Ocean Drilling Program Site 738 in the antarctic Indian Ocean and at Nye Kløv in Denmark. These data suggest that planktic carbonate d13C values in high latitudes may not have decreased dramatically at the K/T boundary; thus, surface-water productivity may not have been reduced as much as in low and middle latitudes. Comparison of the records of Site 738 with those of ODP Sites 690 and 750 indicates a pronounced decline in d13C values of planktic and benthic foraminifera and fine-fraction/bulk carbonate ~200 000 yr after the K/T boundary. This reflects a regional shift in the carbon isotopic composition of oceanic total dissolved carbon (TDC) and correlates with a similar change in benthic foraminiferal d13C values at mid- and low-latitude Deep Sea Drilling Project Sites 527 and 577. This oceanographic event was followed by the ecosystem's global recovery ~500 000 yr after the K/T boundary. These data suggest that the environmental effects of the K/T boundary may have been less severe in the high-latitude oceans than in tropical and subtropical regions.