Global warming leads to Early Triassic nutrient stress across northern Pangea
The largest extinction in Earth history, in the latest Permian, was followed throughout most of
the Early Triassic by a prolonged period of ecologic recovery. What factors delayed biotic …
the Early Triassic by a prolonged period of ecologic recovery. What factors delayed biotic …
Early Triassic productivity crises delayed recovery from world's worst mass extinction
The recovery of life after the latest Permian extinction was protracted over Early Triassic
time. Detailed geochemistry of marine sections along northwest Pangea indicates that …
time. Detailed geochemistry of marine sections along northwest Pangea indicates that …
[HTML][HTML] Continental weathering and recovery from ocean nutrient stress during the Early Triassic Biotic Crisis
J Knies, J Schönenberger, H Zwingmann… - … Earth & Environment, 2022 - nature.com
Following the latest Permian extinction∼ 252 million years ago, normal marine and
terrestrial ecosystems did not recover for another 5-9 million years. The driver (s) for the …
terrestrial ecosystems did not recover for another 5-9 million years. The driver (s) for the …
Recovery from persistent nutrient-N limitation following the Permian–Triassic mass extinction
Global warming, widespread oceanic anoxia and stagnation, and large perturbations of the
global carbon cycle characterized the end-Permian to Middle Triassic interval. Nitrogen …
global carbon cycle characterized the end-Permian to Middle Triassic interval. Nitrogen …
Testing the limits in a greenhouse ocean: Did low nitrogen availability limit marine productivity during the end-Triassic mass extinction?
The end-Triassic mass extinction has been characterized as a 'greenhouse extinction',
related to rapid atmospheric warming and associated changes in ocean circulation and …
related to rapid atmospheric warming and associated changes in ocean circulation and …
[HTML][HTML] Phosphorus cycle and primary productivity changes in the Tethys Ocean during the Permian-Triassic transition: Starving marine ecosystems
J Müller, Y Sun, F Yang, A Fantasia… - Frontiers in Earth …, 2022 - frontiersin.org
The ultimate cause (s) of the end-Permian mass extinction (∼ 252 Ma ago) has been
disputed. A complex interplay of various effects, rather than a single, universal killing …
disputed. A complex interplay of various effects, rather than a single, universal killing …
Water mass denitrification during the latest Permian extinction in the Sverdrup Basin, Arctic Canada
Abstract Late Permian–Early Triassic bulk sedimentary nitrogen isotope (δ15N) and
biomarker data have been generated from the northwest margin of Pangea. Sediments from …
biomarker data have been generated from the northwest margin of Pangea. Sediments from …
δ13C evidence that high primary productivity delayed recovery from end-Permian mass extinction
Euxinia was widespread during and after the end-Permian mass extinction and is commonly
cited as an explanation for delayed biotic recovery during Early Triassic time. This anoxic …
cited as an explanation for delayed biotic recovery during Early Triassic time. This anoxic …
From the warm Pliocene to the cold Pleistocene: A tale of two oceans
GM Filippelli, JA Flores - Geology, 2009 - pubs.geoscienceworld.org
960 GEOLOGY, October 2009 utilization ratio after the end of the Pliocene. One implication
of this is that with enhanced dentrification, there is a consumption of bioavailable nitrate, and …
of this is that with enhanced dentrification, there is a consumption of bioavailable nitrate, and …
Climatic and biotic upheavals following the end-Permian mass extinction
Recovery from the end-Permian mass extinction is frequently described as delayed,,, with
complex ecological communities typically not found in the fossil record until the Middle …
complex ecological communities typically not found in the fossil record until the Middle …