Cyclic anoxia and organic rich carbonate sediments within a drowned carbonate platform linked to Antarctic ice volume changes: Late Oligocene-early Miocene Maldives-Reference-Cited by-同舟云学术

Cyclic anoxia and organic rich carbonate sediments within a drowned carbonate platform linked to Antarctic ice volume changes: Late Oligocene-early Miocene Maldives

Published:2019-09 Issue: Volume:521 Page:1-13
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Swart Peter K.^ORCID,Blättler Clara L.^ORCID,Nakakuni Masatoshi^ORCID,Mackenzie Greta J.,Betzler Christian^ORCID,Eberli Gregor P.,Reolid Jesus,Alonso-García Montserrat,Slagle Angela L.^ORCID,Wright James D.,Kroon Dick,Reijmer John J.G.,Hui Mee Anna L.,Young Jeremy R.,Alvarez-Zarikian Carlos A.^ORCID,Bialik Orr M.^ORCID,Guo Junhua Adam,Haffen Sebastian,Horozal Senay,Inoue Mayuri^ORCID,Jovane Luigi,Lanci Luca^ORCID,Laya Juan Carlos,Lüdmann Thomas,Nagender Nath B.,Niino Kaoru,Petruny Loren M.,Pratiwi Santi Dwi,Su Xiang,Sloss Craig R.,Yao Zhengquan^ORCID

Funder

Portuguese National Science and Technology Foundation

JAMSTEC

Natural History Museum

UKIODP

NERC

NSF

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference51 articles.