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This discrepancy could be attributed to a site- and potentially region-specific under-representation of BC scavenging and associated wet deposition processes in the model
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https://doi.org/10.5194/ACP-26-6741-2026
The Mount Kenya station (MKN), operational since 1999, represents a unique monitoring site in tropical Africa
https://doi.org/10.1038/S41467-026-71959-Y
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https://doi.org/10.1038%2Fs41558-020-00985-5
org
GDP (Current US$) (World Bank, accessed 10 February 2020); https://data
https://dx.doi.org/10.1038/s41586-026-10893-x
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https://dx.doi.org/10.1038/s41586-026-10912-x
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https://doi.org/10.1038/s41597-025-06127-w
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https://doi.org/10.1038%2Fnature08227
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https://doi.org/10.1038%2Fs41586-024-07323-1
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https://doi.org/10.5194/GMD-19-2577-2026
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https://doi.org/10.5194/ACP-26-4509-2026
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https://doi.org/10.5194/acp-22-10173-2022
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https://doi.org/10.1038/s41467-020-16818-0
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https://doi.org/10.1038/srep44095
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https://doi.org/10.5670%2Foceanog.2024.501
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}, volume = {issue_volume}, url = {https://doi
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