2020
DOI: 10.1080/02724634.2020.1803340
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African Land Mammal Ages

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Cited by 34 publications
(19 citation statements)
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“…The three major clades within the Rhinocerotinae subfamily diverged $16 mya (Figure 2A), at the end of the early Miocene and around the time of the Miocene climatic optimum (17-14 mya), a period that was $3 C-4 C warmer than present (Lewis et al, 2008;Sosdian et al, 2020). Diversification occurred after the formation of the terrestrial connection between the Afro-Arabian and Eurasian landmasses $20 mya (Van Couvering and Delson, 2020). We hypothesize that this land bridge enabled dispersal events followed by vicariance, as is well documented with the immigration into Africa from Eurasia of early rhinocerotids, giraffids, suids, and viverrids and the emigration from Africa to Eurasia of apes, deinotheres, and elephantoids, among others (Van Couvering and Delson, 2020).…”
Section: Timing Of Divergence Between Speciesmentioning
confidence: 99%
“…The three major clades within the Rhinocerotinae subfamily diverged $16 mya (Figure 2A), at the end of the early Miocene and around the time of the Miocene climatic optimum (17-14 mya), a period that was $3 C-4 C warmer than present (Lewis et al, 2008;Sosdian et al, 2020). Diversification occurred after the formation of the terrestrial connection between the Afro-Arabian and Eurasian landmasses $20 mya (Van Couvering and Delson, 2020). We hypothesize that this land bridge enabled dispersal events followed by vicariance, as is well documented with the immigration into Africa from Eurasia of early rhinocerotids, giraffids, suids, and viverrids and the emigration from Africa to Eurasia of apes, deinotheres, and elephantoids, among others (Van Couvering and Delson, 2020).…”
Section: Timing Of Divergence Between Speciesmentioning
confidence: 99%
“…Hard minimum bound 37.0 Ma Soft maximum bound 55.8 Ma Age justifications The BQ-2 locality has been correlated with Chron 17n.1n (Seiffert, 2006), which is currently recognized as spanning ~37.5-37.0 Ma (Houben et al, 2019;Agnini et al, 2020), resulting in a minimum bound for this node of 37.0 Ma (see also Van Couvering and Delson, 2020). The maximum bound is based on the maximum age of the earliest well known stem strepsirrhine, Donrussellia provincialis (see "Crown Primates" above), based on the assumption that the divergence of crown Strepsirrhini is unlikely to predate the oldest stem member of the clade.…”
Section: Calibrating Taxon Saharagalago Misrensismentioning
confidence: 99%
“…We assigned a fixed age of 0 Ma to all of our extant taxa. For most of our fossil and subfossil taxa, we assigned uniform age ranges corresponding to the entire possible age range of the specimens used for scoring purposes (following Püschel et al, 2020); however, we assigned a fixed age of 33.4 Ma to Catopithecus and Proteopithecus, all specimens of which are from Quarry L-41 of the Jebel Qatrani Formation in the Fayum Depression of Egypt, which has been assigned an age of 33.4 Ma by Van Couvering and Delson (2020). A full justification of the assigned ages for all of our fossil and subfossil taxa is given in Supplementary Online Material.…”
Section: <Table 1 About Here>mentioning
confidence: 99%
“…2008; O’Leary et al . 2019; Van Couvering & Delson 2020). A precise age is difficult to estimate, although the oolitic limestone of Samit is considered as part of the Tamaguélelt Formation that spans the Ypresian (early Eocene) (O’Leary et al .…”
Section: Geological Settingmentioning
confidence: 99%