Early precambrian banded iron formations: Biochemical precipitates from highly evaporated hydrothermal solutions of polar region lakes
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/BF03228053.pdf
Reference79 articles.
1. SpecialPublication of International Association of Sedimentologists;W. Altermann,2002
2. Developments in Precambrian Geology;W. Altermann,2004
3. ALTERMANN, W. and CORCORAN, P., 2002, Precambrian Sedimentary Environments: A modern approach to ancient depositional systems. Blackwell, Oxford, 464 p.
4. ALTERMANN, W. and HERBIG, H.G., 1991, Tidal flat deposits of the Lower Proterozoic Campbell Group along the southwestern margin of the Kaapvaal Craton, Northern Cape Province: South African Journal of Earth Sciences, v. 13, p. 415–435.
5. AWRAMIK, S.M., 1992, The oldest records of photosynthesis: Photosynthesis Research, v. 33, p. 75–89.
Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Genesis: early life survived in the Polar Circles by precipitating banded iron formation (~ 3.7–1.85 Ga) followed by stratified ferruginous siliciclasts until ~ 580 Ma, when tectonically shifted to lower latitudes initiating the ‘Cambrian Explosion’;International Journal of Earth Sciences;2022-05-18
2. Varves in marine sediments: A review;Earth-Science Reviews;2016-08
3. Biotic and abiotic oxidation and reduction of iron at circumneutral pH are inseparable processes under natural conditions;Geomicrobiology Journal;2015-03-16
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