Details
| Original language | English |
|---|---|
| Title of host publication | Iron Geochemistry |
| Subtitle of host publication | An Isotopic Perspective |
| Place of Publication | Cham |
| Publisher | Springer Nature |
| Pages | 215-360 |
| Number of pages | 146 |
| ISBN (electronic) | 9783030338282 |
| ISBN (print) | 9783030338275 |
| Publication status | Published - 10 Jan 2020 |
Publication series
| Name | Advances in Isotope Geochemistry |
|---|---|
| ISSN (Print) | 2364-5105 |
| ISSN (electronic) | 2364-5113 |
Abstract
Much of Chap. 5 focused on the fluid envelope of various surface environments in the modern Earth, where Fe redox changes, organic complexation, and mineral precipitation produce large changes in Fe isotope compositions of fluids and minerals. As we step into the ancient Earth, we lose the ability to measure fluids directly, yet the fluid envelope remained a key component of the Fe biogeochemical cycle in Earth’s past, especially in an anoxic Earth when large quantities of (formula presented) existed in the oceans.
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Geochemistry and Petrology
- Chemistry(all)
- Spectroscopy
Sustainable Development Goals
Cite this
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Iron Geochemistry: An Isotopic Perspective. Cham: Springer Nature, 2020. p. 215-360 (Advances in Isotope Geochemistry).
Research output: Chapter in book/report/conference proceeding › Contribution to book/anthology › Research › peer review
}
TY - CHAP
T1 - The ancient earth
AU - Johnson, Clark
AU - Beard, Brian
AU - Weyer, Stefan
PY - 2020/1/10
Y1 - 2020/1/10
N2 - Much of Chap. 5 focused on the fluid envelope of various surface environments in the modern Earth, where Fe redox changes, organic complexation, and mineral precipitation produce large changes in Fe isotope compositions of fluids and minerals. As we step into the ancient Earth, we lose the ability to measure fluids directly, yet the fluid envelope remained a key component of the Fe biogeochemical cycle in Earth’s past, especially in an anoxic Earth when large quantities of (formula presented) existed in the oceans.
AB - Much of Chap. 5 focused on the fluid envelope of various surface environments in the modern Earth, where Fe redox changes, organic complexation, and mineral precipitation produce large changes in Fe isotope compositions of fluids and minerals. As we step into the ancient Earth, we lose the ability to measure fluids directly, yet the fluid envelope remained a key component of the Fe biogeochemical cycle in Earth’s past, especially in an anoxic Earth when large quantities of (formula presented) existed in the oceans.
UR - http://www.scopus.com/inward/record.url?scp=85078081126&partnerID=8YFLogxK
U2 - 10.1007/978-3-030-33828-2_6
DO - 10.1007/978-3-030-33828-2_6
M3 - Contribution to book/anthology
AN - SCOPUS:85078081126
SN - 9783030338275
T3 - Advances in Isotope Geochemistry
SP - 215
EP - 360
BT - Iron Geochemistry
PB - Springer Nature
CY - Cham
ER -