James V. Browning

TL;DR: Long-term sea level peaked at 100 ± 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred, and presents a new sea-level record for the past 100 million years.

TL;DR: In this article, the authors present a method for estimating sea level for the last 108 million years through backstripping of corehole data from the New Jersey and Delaware Coastal Plains.

TL;DR: In this paper, the authors reconcile records of warm high latitudes with glacio-eustasy by proposing that Late Cretaceous-early Eocene ice sheets generally reached maximum volumes of 8 −12 −10 6 km 3 (20 −30 m glacioeustatic equivalent), but did not reach the Antarctic coast; hence, coastal Antarctica remained relatively warm even though there were significant changes in sea level as the result of glaciation.

TL;DR: The New Jersey Sea Level Transect was designed to evaluate the relationships among global sea level (eustatic) change, unconformity-bounded sequences, and variations in subsidence, sediment supply, and climate on a passive continental margin this article.

TL;DR: This paper provided a record of global sea-level (eustatic) variations of the Late Cretaceous (99- 65 Ma) greenhouse world, showing that sea level changes were large (25 m) and rapid (K 1 m).