A large (30-40 m), rapid (≪1 m.y.), earliest Maastrichtian sealevel drop inferred from New Jersey sequence stratigraphic records correlates with synchronous δ18O increases in deep-water benthic and low-latitude surface-dwellin planktonic foraminifera. The coincidence of these events argues for the development of a moderate-sized ice sheet during the early Maastrichtian.
CITATION STYLE
Miller, K. G., Barrera, E., Olsson, R. K., Sugarman, P. J., & Savin, S. M. (1999). Does ice drive early Maastrichtian eustasy? Geology, 27(9), 783–786. https://doi.org/10.1130/0091-7613(1999)027<0783:DIDEME>2.3.CO;2
Mendeley helps you to discover research relevant for your work.