dc.contributor.author |
Swanner, Elizabeth D. |
|
dc.contributor.author |
Maisch, Markus |
|
dc.contributor.author |
Wu, Wenfang |
|
dc.contributor.author |
Kappler, Andreas |
|
dc.date.accessioned |
2019-11-14T12:45:42Z |
|
dc.date.available |
2019-11-14T12:45:42Z |
|
dc.date.issued |
2018 |
|
dc.identifier.issn |
2045-2322 |
|
dc.identifier.uri |
http://hdl.handle.net/10900/94779 |
|
dc.language.iso |
en |
en |
dc.publisher |
Nature Publishing Group |
de_DE |
dc.relation.uri |
http://dx.doi.org/10.1038/s41598-018-22694-y |
|
dc.subject.ddc |
500 |
de_DE |
dc.title |
Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater |
de_DE |
dc.type |
Article |
de_DE |
utue.quellen.id |
20190321153956_03326 |
|
utue.personen.roh |
Swanner, Elizabeth D. |
|
utue.personen.roh |
Maisch, Markus |
|
utue.personen.roh |
Wu, Wenfang |
|
utue.personen.roh |
Kappler, Andreas |
|
dcterms.isPartOf.ZSTitelID |
Scientific Reports |
de_DE |
dcterms.isPartOf.ZS-Issue |
Article 4238 |
de_DE |
dcterms.isPartOf.ZS-Volume |
8 |
de_DE |
utue.fakultaet |
07 Mathematisch-Naturwissenschaftliche Fakultät |
|