Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4748852 | Marine Micropaleontology | 2014 | 8 Pages |
Abstract
A more significant time transgressive increase in Shallow and Others radiolarian Assemblage flux occurs initially in the southernmost core in mid-Holocene, ultimately recorded at the northernmost site during the late Holocene. Here flux of the Deep Assemblage and C. davisiana also increases.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Palaeontology
Authors
J.J. Morley, J.D. Hays,