In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 36, No. 2 ( 2021-02)
Kurzfassung:
Cyclostratigraphy applied to two Eocene Indian Ocean scientific drilling records reveals the fingerprint of orbital eccentricity Sedimentary noise at both sites contains a 1.2‐Myr obliquity imprint, albeit in antiphase: Mechanisms causing noise are thus different While sea‐level change causes noise at shallower sites, bottom current intensity might introduce sedimentary noise at deep‐ocean sites
Materialart:
Online-Ressource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2020PA004116
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2021
ZDB Id:
2916554-4