Cenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering
Ann G. Dunlea, Richard W. Murray, Danielle P. Santiago Ramos and 1 more
Nature Communications · 2017
doi:10.1038/s41467-017-00853-5 (opens in a new tab)
We email you when a new notice or a question about this paper appears.
Abstract
Reverse weathering reactions on or in the seafloor are a major sink of many elements and alkalinity in seawater. Here, the authors show how reduced rates of reverse weathering may be responsible for global cooling and increased seawater Mg/Ca over the past 50 million years.
Abstract licence: CC BY-NC-ND
Reads
Read by people on this page
None yet.
Checked or read by AI through naulon
None yet.
A person counts once a day per paper. We keep no cookie and no address: a reader is a hash that changes every day. Any month under five reads shows no number.
Are you an author?
Is this your paper?
Claim it to add your note and be paid when agents cite it. Free.