Distinguishing between oxygen and substrate control in fossil benthic assemblages
- 1 January 1993
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 150 (1), 193-196
- https://doi.org/10.1144/gsjgs.150.1.0193
Abstract
No abstract availableThis publication has 12 references indexed in Scilit:
- The Callovian-Oxfordian boundary in Oxfordshire and Wiltshire based on two new temporary sectionsProceedings of the Geologists' Association, 1992
- Faunal response to transgressive-regressive cycles: example from the Jurassic of western IndiaPalaeogeography, Palaeoclimatology, Palaeoecology, 1991
- Oxygen-related biofacies in marine strata: an overview and updateGeological Society, London, Special Publications, 1991
- The Lower Oxford Clay: production and preservation of organic matter in the Callovian (Jurassic) of central EnglandGeological Society, London, Special Publications, 1991
- Palaeoenvironments of the Nordenskjöld Formation: an Antarctic Late Jurassic—Early Cretaceous black shale-tuff sequenceGeological Society, London, Special Publications, 1991
- Carbonate Substrates of the Late Cretaceous Sea, Central Great Plains and Southern Rocky MountainsPALAIOS, 1986
- Erosion, transport and deposition of fine-grained marine sedimentsGeological Society, London, Special Publications, 1984
- Comparison of major sequences of organic-rich mud deposition in the British JurassicJournal of the Geological Society, 1980
- Functional morphology and palaeontological significance of the conchiolin layers in corbulid pelecypodsLethaia, 1979
- EVOLUTIONARY AND ECOLOGIC SIGNIFICANCE OF OXYGEN‐DEFICIENT MARINE BASINSLethaia, 1971