Lawrence Flynn

Dr. Lawrence Flynn

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Research Focus & Metrics

Academic Career Length

42Years (1985-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 September 2016 in Comptes Rendus Palevol
Verified
Journal Article
Closed access
LFLawrence Flynn
Lawrence Flynn
DPDavid Pilbeam
David Pilbeam
JBJohn C. Barry
John C. Barry
MMMichèle E. Morgan
Michèle E. Morgan
SRS. Mahmood Raza
S. Mahmood Raza

31 October 2013 in Mammal Review
Verified
Journal Article
Closed access
PDF file
LFLawrence Flynn
Lawrence Flynn
AWAlisa J. Winkler
Alisa J. Winkler
MEMargarita Erbaeva
Margarita Erbaeva
NANadia Alexeeva
Nadia Alexeeva
UAUlrike Anders
Ulrike Anders
ZZZhao-Qun Zhang
Zhao-Qun Zhang

14 May 2013
Verified
Book Chapter
Closed access
LFLawrence Flynn
Lawrence Flynn
ELEverett H. Lindsay
Everett H. Lindsay
DPDavid Pilbeam
David Pilbeam
SRS. Mahmood Raza
S. Mahmood Raza
MMMichèle E. Morgan
Michèle E. Morgan
NONeil D. Opdyke
Neil D. Opdyke

24 October 2012 in Cladistics
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Journal Article
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RLRaquel López-Antoñanzas
Raquel López-Antoñanzas
LFLawrence Flynn
Lawrence Flynn
Fabien KnollFabien Knoll
Fabien Knoll
The subfamily Rhizomyinae is known from the Late Oligocene up to the present. Today this group comprises six species, which live in southern Asia and eastern Africa. Despite the current moderate diversity of the rhizomyines, they had a greater diversification and wider distribution in the past: from Asia, their land of origin, to Africa, which they entered during the Early Miocene. So far 33 fossil species can be referred to this group. A cladistic analysis involving fossil and living species has been carried out. Prokanisamys spp. turned out to be the most basal taxa of the ingroup. This analysis calls into question the monophyly of several genera, and allows the proposal of a phylogenetic definition of the tribes Tachyoryctini and Rhizomyini. It also provides information about the origin of the African rhizomyines and allows inferring multiple dispersal phenomena from Asia to Africa in Early and Late Miocene times.

1 August 2017 in Fossil Imprint
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Journal Article
Open access
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YKYuri Kimura
Yuri Kimura
LFLawrence Flynn
Lawrence Flynn
LJLouis L. Jacobs
Louis L. Jacobs
The early late Miocene is an interval of increased diversification for murine rodents. Whereas the genus Progonomys became widespread throughout Eurasia by 10 Ma, it appears from the known paleontological record that southern Asia is the arena of evolution and diversification at the base of the Murinae. The Siwalik fossil record of the Potwar Plateau in northern Pakistan preserves fossil evidence relevant to unraveling this history. Murine rodents are recorded there throughout the middle Miocene, and diversification began in Siwalik assemblages before 11 Ma. The well-established Progonomys and Karnimata lineages were already present between 11 and 10 Ma, and these represent extant murine crown groups. Here we document diversity in Siwalik murines dating to 10.5 to 10.1 Ma, and clarify their recognition by naming a new species of Karnimata and referring specimens of Progonomys from this interval to P. hussaini. In addition, we define at least two other uncommon murine species that coexist with them. One of these is an early record of Parapodemus, a fossil genus of Tribe Apodemurini, which constitutes a calibration point for the Apodemus/Tokudaia split. Together, these fossil taxa provide further evidence bearing on the major split among murines leading to the clades Murini and Arvicanthini.

1 September 2020 in Journal of Human Evolution
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Journal Article
Open access
NJNina Jablonski
Nina Jablonski
XJXueping Ji
Xueping Ji
JKJay Kelley
Jay Kelley
LFLawrence Flynn
Lawrence Flynn
CDChenglong Deng
Chenglong Deng
DSDenise F. Su
Denise F. Su
A dentate mandible and proximal femur of Mesopithecus pentelicusWagner, 1839 are described from the Shuitangba lignite mine in Zhaotong Prefecture, northeastern Yunnan Province, China. The remains were retrieved from sediments just below those that yielded a juvenile Lufengpithecus cranium and are dated at about ∼6.4 Ma. The mandible and proximal femur were found in close proximity and are probably of the same individual. The lower teeth are metrically and morphologically closely comparable with those of confirmed M. pentelicus from Europe, and on this basis, the specimen is assigned to this species. The anatomy of the proximal femur indicates that the Shuitangba Mesopithecus was a semiterrestrial quadruped that engaged in a range of mostly arboreal activities, including walking, climbing, and occasional leaping, with an abducted hip joint. The Shuitangba Mesopithecus is dentally typical for the genus but may have been more arboreal than previously described for M. pentelicus. M. pentelicus is well known from late Miocene (MN 11-12) sites in Europe and southwest Asia. Its estimated average rate of dispersal eastward was relatively slow, although it could have been episodically more rapid. The presence of a colobine, only slightly lower in the same section at Shuitangba that produced Lufengpithecus, is one of the only two well-documented instances of the near or actual co-occurrence of a monkey and ape in the Miocene of Eurasia. At Shuitangba, M. pentelicus occupied a freshwater-margin habitat with beavers, giant otters, swamp rabbits, and many aquatic birds. The presence of M. pentelicus in southwest China near the end of the Miocene further attests to the ecological versatility of a species long recognized as widespread and adaptable. The modern colobines of Asia, some or all of which are probable descendants of Mesopithecus, have gone on to inhabit some of the most highly seasonal and extreme habitats occupied by nonhuman primates.