2021
DOI: 10.1016/j.revpalbo.2021.104456
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Fossil infructescence from southwestern China reveals Paleogene establishment of Cladrastis in Asia

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Cited by 9 publications
(2 citation statements)
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“…Central Tibet, a valley surrounded by high northern and southern mountains (Ding et al ., 2014, 2022; Su et al ., 2019a, 2020; Spicer et al ., 2020, 2021; Xiong et al ., 2023), likely played an important role in the floristic exchange of the Northern Hemisphere during the Paleogene (late Eocene to early Oligocene) (Del Rio et al ., 2020; Li et al ., 2022; Liu et al ., 2022). This valley has yielded a succession of radiometrically diverse fossil flora that have shown biological connections to newly docked India, North America, and Europe as well as the first occurrence of several taxa that are now part of the EAEBLFs (Liu et al ., 2019; Tang et al ., 2019; Su et al ., 2019b, 2020; Del Rio et al ., 2020, 2022; Jia et al ., 2021, 2022; Chen et al ., 2022; Li et al ., 2022; Zhang et al ., 2022). Additionally, the Pan Gulf of Tonkin flora (Huang et al ., 2022), which may be an important source for the post‐Paleogene East Asian arid belt retreat, suggests that accumulation may have started from the late Eocene to early Oligocene.…”
Section: Discussionmentioning
confidence: 99%
“…Central Tibet, a valley surrounded by high northern and southern mountains (Ding et al ., 2014, 2022; Su et al ., 2019a, 2020; Spicer et al ., 2020, 2021; Xiong et al ., 2023), likely played an important role in the floristic exchange of the Northern Hemisphere during the Paleogene (late Eocene to early Oligocene) (Del Rio et al ., 2020; Li et al ., 2022; Liu et al ., 2022). This valley has yielded a succession of radiometrically diverse fossil flora that have shown biological connections to newly docked India, North America, and Europe as well as the first occurrence of several taxa that are now part of the EAEBLFs (Liu et al ., 2019; Tang et al ., 2019; Su et al ., 2019b, 2020; Del Rio et al ., 2020, 2022; Jia et al ., 2021, 2022; Chen et al ., 2022; Li et al ., 2022; Zhang et al ., 2022). Additionally, the Pan Gulf of Tonkin flora (Huang et al ., 2022), which may be an important source for the post‐Paleogene East Asian arid belt retreat, suggests that accumulation may have started from the late Eocene to early Oligocene.…”
Section: Discussionmentioning
confidence: 99%
“…Legumes also have an abundant and diverse fossil record, with numerous fossil flowers, fruits, and leaves documented from the Cenozoic of every continent except Antarctica (Herendeen, 1992 ; Herendeen and Dilcher, 1992 ; Herendeen et al, 1992 ). Temporal and biogeographic patterns in the fossil record of the family were summarized by Herendeen et al ( 1992 ), to which have been added more recent fossil reports from low paleolatitude localities, mainly in Africa and Central and South America (Herendeen and Jacobs, 2000 ; De Franceschi and De Ploëg, 2003 ; Jacobs and Herendeen, 2004 ; Calvillo‐Canadell and Cevallos‐Ferriz, 2005 ; Brea et al, 2008 ; Wing et al, 2009 ; Pan et al, 2010 , 2012 ; Collinson et al, 2012 ; Cantrill et al, 2013 ; Jia and Manchester, 2014 ; Shukla and Mehrotra, 2016 ; Herendeen and Herrera, 2019 ; Herrera et al, 2019 ; Lyson et al, 2019 ; Shukla et al, 2019 ; Jia et al, 2021 ; Li et al, 2021 ). By the middle Eocene all major lineages within the family are documented in the fossil record, and many securely identified fossils have been used to calibrate branch ages from molecular phylogenetic analyses (Herendeen et al, 1992 ; Lavin et al, 2005 ; Bruneau et al, 2008 ; Magallon et al, 2015 ; Estrella et al, 2017 ; Koenen et al, 2021 ).…”
mentioning
confidence: 99%