Pliocene peak sea level and warmth: Integration of a Virginia corehole array and deep-sea isotope and trace metal records

Rutgers University New Brunswick, New Brunswick NJ

Investigators

Abstract

PIs promise to establish the sea level rise associated with warm Pliocene high stands. This is critical to our understanding of the cryosphere during a time that has been suggested by many to be similar in some respects to conditions expected by the end of this century.