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Benthic foraminiferal dissolved-oxygen index and dissolved-oxygen levels in the modern ocean
Changes in oxygen concentrations at the sediment-water interface play a major role in controlling benthic foraminiferal assemblages and morphologic characteristics; such changes are reflected inExpand
Survival strategies of brachiopod faunas from the end-Permian mass extinction
Abstract Global reviews reveal that 102 brachiopod species (including 40 indeterminate species) belonging to 43 genera within 27 families survived the end-Permian mass extinction in South China, theExpand
Latest Paleocene benthic foraminiferal extinction and environmental changes at Tawanui, New Zealand
A major extinction of intermediate-water (500–1000 m) benthic foraminiferal species coincided with a major decrease in δ13C (2.8‰) of terrestrial organic matter (n-C29 alkane) and δ34S (20‰) of wholeExpand
Early Triassic recovery of the brachiopod faunas from the end-Permian mass extinction: A global review
Abstract Brachiopod faunas in Lower Triassic deposits from Spitzbergen, Primorye of Russia, Japan, Mangyslak of Kazakhstan, Alpine Europe, the Caucasus, the Middle East, the Himalaya, South China,Expand
Global changes of Paleogene aerobic/anaerobic benthic foraminifera and deep-sea circulation
Kaiho, K., 1991. Cenozoic global changes of aerobic/anaerobic benthic foraminifera and deep-sea circulation. Palaeogeogr., Palaeoclimalol., Palaeoecol., 83: 65-85. Morphologies of calcareous benthicExpand
Effect of organic carbon flux and dissolved oxygen on the benthic foraminiferal oxygen index (BFOI)
Variations in oceanic primary productivity, flux of organic carbon to the sediments, and dissolved-oxygen levels in the water column are thought to be important in the control of benthicExpand
Timing and magnitude of early Aptian extreme warming: Unraveling primary δ18O variation in indurated pelagic carbonates at Deep Sea Drilling Project Site 463, central Pacific Ocean
Abstract In order to elucidate early Aptian marine paleotemperature evolution across the period of enhanced organic carbon (Corg)-burial [Oceanic Anoxic Event (OAE) 1a], stable isotope analyses wereExpand
Oceanic crust production and climate during the last 100 Myr
In order to evaluate the possible influence of oceanic crust production on climatic changes during the past 100Myr variations in total oceanic crust for this period including production at mid-oceanExpand
Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China
This paper describes fourteen brachiopod species in eleven genera from the Late Permian Wuchiapingian Coal Series (Lungtan Formation) of South China. Of these, the shell bed fauna from the basalExpand
Oceanic primary productivity and dissolved oxygen levels at the Cretaceous/Tertiary Boundary: Their decrease, subsequent warming, and recovery
Thirty-six different geochemical and foraminiferal analyses were conducted on samples collected at closely spaced intervals across the Cretaceous/Tertiary (K/T) boundary exposed at Caravaca, Spain. AExpand
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