Journal ArticleDOI
The TICE event: Perturbation of carbon–nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse–icehouse transition
Le Yao,Wenkun Qie,Genming Luo,Jiangsi Liu,Thomas J. Algeo,Thomas J. Algeo,Xiao Bai,Bo Yang,Xiangdong Wang +8 more
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TLDR
The mid-Tournaisian carbon isotope excursion (TICE) as discussed by the authors was probably triggered by an increase in organic carbon burial rates linked to changes in global ocean circulation.About:
This article is published in Chemical Geology.The article was published on 2015-04-24. It has received 50 citations till now.read more
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The impacts of land plant evolution on Earth's climate and oxygenation state ─ An interdisciplinary review
Tais W. Dahl,Susanne K. M. Arens +1 more
TL;DR: In this article, the authors review hypotheses and evidence for how the evolving terrestrial ecosystems impacted atmospheric and oceanic O2 and CO2 from the Ordovician and into the Carboniferous (485-298.9 Ma).
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Greenhouse to icehouse: a biostratigraphic review of latest Devonian-Mississippian glaciations and their global effects
TL;DR: This paper assess the primary biostratigraphic and sedimentological data constraining diamictite deposits through the Late Palaeozoic Ice Age (LPIA) and compare these data to the wider record of eustasy, mass extinction and isotope stratigraphy in the lower palaeolatitudes.
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Global events of the Late Paleozoic (Early Devonian to Middle Permian): A review
TL;DR: The Late Paleozoic (Early Devonian to Middle Permian) was an interval of profound changes in Earth-surface systems, reflected in dynamic interplay among the biosphere, hydrosphere, atmosphere, and geosphere as discussed by the authors.
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Ice volume and paleoclimate history of the Late Paleozoic Ice Age from conodont apatite oxygen isotopes from Naqing (Guizhou, China)
TL;DR: A high-resolution and continuous conodont apatite oxygen isotope record spanning the late Visean to Middle Permian is reported from South China, which is interpreted with respect to the ice volume and/or tropical seawater temperature history of the Late Paleozoic Ice Age (LPIA).
Journal ArticleDOI
Climatic and hydrologic controls on upper Paleozoic bauxite deposits in South China
Wenchao Yu,Thomas J. Algeo,Thomas J. Algeo,Jiaxin Yan,Jianghai Yang,Yuansheng Du,Xing Huang,Shenfu Weng +7 more
TL;DR: In this article, a unique combination of geographic, climatic, and eustatic factors accounted for widespread formation of bauxite in South China during the Late Paleozoic Ice Age (LPIA).
References
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Journal ArticleDOI
Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
TL;DR: This work focuses primarily on the periodic and anomalous components of variability over the early portion of this era, as constrained by the latest generation of deep-sea isotope records.
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An Earth-system perspective of the global nitrogen cycle.
Nicolas Gruber,James N. Galloway +1 more
TL;DR: With humans having an increasing impact on the planet, the interactions between the nitrogen cycle, the carbon cycle and climate are expected to become an increasingly important determinant of the Earth system.
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Preservation of elemental and isotopic source identification of sedimentary organic matter
TL;DR: The amount and type of organic matter in the sediments of lakes and oceans contribute to their paleoenvironmental and paleoclimatological records as discussed by the authors, but only a small fraction of the initial aquatic organic matter survives destruction and alteration during sinking and sedimentation.
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The evolution and future of earth's nitrogen cycle
TL;DR: Humans must modify their behavior or risk causing irreversible changes to life on Earth, as the damage done by humans to the nitrogen economy of the planet will persist for decades, possibly centuries, if active intervention and careful management strategies are not initiated.
Journal ArticleDOI
Anoxic Environments and Oil Source Bed Genesis
TL;DR: The anoxic aquatic environment is a mass of water so depleted in oxygen that virtually all aerobic biologic activity has ceased as discussed by the authors, where the demand for oxygen in the water column exceeds the supply.