Cited by 63Paleontology and Stratigraphy of FossilsGeological formations and processesGeology and Paleoclimatology Research

Time-specific black mudstones and global hyperwarming on the Cambrian–Ordovician slope and shelf of the Laurentia palaeocontinent

Landing, Ed·2012·Palaeogeography, Palaeoclimatology, Palaeoecology

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Crossref · 10.1016/j.palaeo.2011.09.005

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6 of 6 references verified0 citation errors · 0 not checkable

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  • Carbonate precipitation may have been further influenced locally by flooding of bicarbonate-rich anoxic water masses onto the continents during transgressions and by the high temperatures of epicratonic seaways lying at low latitudes.

    “In addition, carbonate precipitation may have been further influenced locally by flooding of bicarbonate-rich anoxic water masses onto the continents during transgressions (26) and by the high temperatures of epicratonic seaways lying at low latitudes (27).”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [27]

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Authors
Landing, E.
Affiliations
New York State Museum (US)
Corresponding author
Landing, Ed
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2012-12
Volume
367-368
Pages
256-272
ISSN
0031-0182 (ISSN-L)
OpenAlex
W2084724673
Cited by
63
References
6
Citations by year
2025: 5 · 2024: 4 · 2023: 9 · 2022: 5 · 2021: 8 · 2020: 2 · 2019: 2 · 2018: 9 · 2017: 2 · 2016: 2 · 2015: 5 · 2014: 1 · 2013: 4 · 2012: 5
FWCI
2.02
Type
journal article
Language
en
Open access
closed
Locations
Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion)
Funders
National Science Foundation
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Keywords
black mudstone, eustatic sea-level rise, Cambrian-Ordovician, Late Ordovician, Late Devonian, greenhouse microclimate, thermal expansion, deep ocean circulation, oxygen solubility, sea-level change, Phanerozoic climate

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