Skip to Main Content
Skip Nav Destination


Examination of the benthic foraminifera from the northwestern Gulf of Mexico slope (90–95o W; 283–1341 m) reveals widespread changes in their assemblages during the transition from the most recent sea-level lowstand (last glacial maximum) to the current highstand (interglacial). These glacial assemblages are defined by Q-mode cluster and R-mode principal component analyses of both relative abundance and presence/absence data from 61 samples dated at 15 ka. Distinct bathymetric positions can be assigned to the assemblages, except in the case of a deltaic outflow assemblage. They are interpreted to be associated with water masses, and basin-wide changes in water-mass position and chemistry at the glacial–postglacial transition are reflected in assemblage changes. Most important is the switch from North Atlantic Intermediate Water (NAIW), which was found in the Gulf during the last glacial maximum, to Subantarctic Intermediate Water (SAIW), which is found in the modern Gulf. This water-mass shift allowed several species associated with SAIW (e.g., Bulimina alazanensis and Osangularia culter) to reenter the Gulf after the last glacial interval. The position of several water-mass boundaries were found to differ between the two time periods, causing the upper depth limits of some species to change with time. The benthic foraminiferal record in a core (water depth 726 m) shows three faunal events during and after the deglaciation; apparently, these events are related to water-mass shifts at 13 and 11 ka and a change in the substrate organic matter at 4.5 ka.

You do not currently have access to this chapter.

Figures & Tables





Citing Books via

Close Modal

or Create an Account

Close Modal
Close Modal