Articles | Volume 18, issue 2
https://doi.org/10.1144/jm.18.2.125
https://doi.org/10.1144/jm.18.2.125
01 Dec 1999
 | 01 Dec 1999

Palaeoenvironment of Maastrichtian ostracods from ODP Holes 1049B, 1050C and 1052E in the Western North Atlantic

Stefan Majoran

Cited articles

E., Barrera: Global environmental changes preceding the Cretaceous–Tertiary boundary: Early–late Maastrichtian transition, Geology, 22, 877-880, 1994.
E., Barrera and B. T., Huber: Evolution of Antarctic waters during the Maastrichtian: foraminifer oxygen and carbon isotope ratios, Leg 113, Proceedings of the Ocean Drilling Program, Scientific Results, 113, 813-827, 1990.
E., Barrera, S. M., Salvin and S., Thomas: Evidence for thermohaline-circulation reversals controlled by sea-level change in the latest Cretaceous, Geology, 25, 715-718, 1997.
R. H., Benson: The origin of the psychrosphere as recorded in changes of deep-sea ostracode assemblages, Lethaia, 8, 69-83, 1975.
R. H., Benson: The Cenozoic Ostracode faunas of the Sao Paulo Plateau and the Rio Grande Rise (DSDP Leg 39, Sites 356 and 357), Initial Reports of the Deep Sea Drilling Project, 39, 869-883, 1977.
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