The biogeochemistry of ferruginous lakes and past ferruginous oceans
ED Swanner, N Lambrecht, C Wittkop, C Harding… - Earth-Science …, 2020 - Elsevier
Anoxic and iron-rich (ferruginous) conditions prevailed in the ocean under the low-oxygen
atmosphere that occurred through most of the Archean Eon. While euxinic conditions (ie …
atmosphere that occurred through most of the Archean Eon. While euxinic conditions (ie …
Identifying oxygen minimum zone-type biogeochemical cycling in Earth history using inorganic geochemical proxies
F Scholz - Earth-Science Reviews, 2018 - Elsevier
Because of anthropogenic global warming, the world ocean is currently losing oxygen. This
trend called ocean deoxygenation is particularly pronounced in low-latitude upwelling …
trend called ocean deoxygenation is particularly pronounced in low-latitude upwelling …
Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction
Explaining the~ 5-million-year delay in marine biotic recovery following the latest Permian
mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for …
mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for …
Oxygenation of the Mesoproterozoic ocean and the evolution of complex eukaryotes
Abstract The Mesoproterozoic era (1,600–1,000 million years ago (Ma)) has long been
considered a period of relative environmental stasis, with persistently low levels of …
considered a period of relative environmental stasis, with persistently low levels of …
[HTML][HTML] The onset of widespread marine red beds and the evolution of ferruginous oceans
Banded iron formations were a prevalent feature of marine sedimentation~ 3.8–1.8 billion
years ago and they provide key evidence for ferruginous oceans. The disappearance of …
years ago and they provide key evidence for ferruginous oceans. The disappearance of …
Cycles of~ 32.5 My and~ 26.2 My in correlated episodes of continental flood basalts (CFBs), hyper-thermal climate pulses, anoxic oceans, and mass extinctions over …
Potential temporal and causal connections among various geologic events have long been
discussed in the geological literature. More recently, signs of common periodicities in these …
discussed in the geological literature. More recently, signs of common periodicities in these …
Two-stage marine anoxia and biotic response during the Permian–Triassic transition in Kashmir, northern India: pyrite framboid evidence
Although expanded ocean anoxia has long been believed to be a direct killing mechanism
causing mortality of organisms during the Permian-Triassic mass extinction, little has been …
causing mortality of organisms during the Permian-Triassic mass extinction, little has been …
The Smithian/Spathian boundary (late Early Triassic): A review of ammonoid, conodont, and carbon-isotopic criteria
The transition from the Smithian substage to the Spathian substage of the Olenekian stage
of the late Early Triassic was a critical time marked by a series of biological and …
of the late Early Triassic was a critical time marked by a series of biological and …
Innovation not recovery: dynamic redox promotes metazoan radiations
R Wood, DH Erwin - Biological Reviews, 2018 - Wiley Online Library
Environmental fluctuations in redox may reinforce rather than hinder evolutionary transitions,
such that variability in near‐surface oceanic oxygenation can promote morphological …
such that variability in near‐surface oceanic oxygenation can promote morphological …
Establishing the link between Permian volcanism and biodiversity changes: Insights from geochemical proxies
Current understanding of biodiversity changes in the Permian is presented, especially the
consensus and disagreement on the tempo, duration, and pattern of end-Guadalupian and …
consensus and disagreement on the tempo, duration, and pattern of end-Guadalupian and …