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https://doi.org/10.1038%2Fs41467-022-32552-1
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https://doi.org/10.1038%2Fs41598-019-45349-y
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https://doi.org/10.1038%2Fs41591-024-03094-4
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https://dx.doi.org/10.1038/s41586-026-10876-y
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https://doi.org/10.1038%2Fncomms16101
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https://doi.org/10.3389/feart.2021.680051
Volcanology
Volume 9 - 2021 | https://doi
https://doi.org/10.5194/ACP-26-4509-2026
In equatorial Africa, both biomass burning and temperature can explain isoprene variability during different periods, representing an intermediate regime with contributions from emissions and chemistry
https://doi.org/10.24972%2Fijts.2002.21.1.145
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https://doi.org/10.3389%2Ffnhum.2014.00020
state of a system but it can also imply physical qualities, where high entropy is synonymous with high disorder
https://doi.org/10.1038%2Fsrep38939
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https://doi.org/10.20341%2Fgb.2023.002
The “Mo Clay” (= Fur Formation, Denmark) and “Turkmenia” (Danata Formation, Turkmenistan) localities, thought by Patterson to date to the late Paleocene, are now known to be early Eocene in age, while the Nardò sites likely lie well within the Campanian