Paleoenvironmental changes associated with the Paleocene-Eocene thermal maximum, Millville (ODP Leg 1&4AX), New Jersey coastal plain
The Paleocene-Eocene Thermal Maximum (PETM) was an abrupt warming of about 5°C that lasted ~1&0-220 kyr. The PETM is recognized by the Carbon Isotope Excursion (CIE), represented by a ~2.5-4 ‰ decrease in planktonic foraminiferal δ13C values in open ocean cores (Kennett and Stott, 1991; Zachos e...
| Main Author: | |
|---|---|
| Format: | Text |
| Language: | unknown |
| Published: |
No Publisher Supplied
2014
|
| Subjects: | |
| Online Access: | https://dx.doi.org/10.7282/t3zc80z5 https://rucore.libraries.rutgers.edu/rutgers-lib/42422/ |