TY - CHAP
T1 - Leaving Gondwana
T2 - the changing position of the Indian subcontinent in the global faunal network
AU - Halliday, Thomas J. D.
AU - Holroyd, Patricia A.
AU - Gheerbrant, Emmanuel
AU - Prasad, Guntupalli V.R.
AU - Scanferla, Agustin
AU - Beck, Robin M.D.
AU - Krause, David W.
AU - Goswami, Anjali
PY - 2020/11/24
Y1 - 2020/11/24
N2 - The paleogeographic history of the Indian subcontinent is unique among Earth’s landmasses. From being part of the southern supercontinent Gondwana for most of the Mesozoic, through a period of isolation as a drifting entity in the Late Cretaceous, to colliding with Asia near the Paleocene-Eocene boundary, the Indian subcontinent has been associated with, and dissociated from, a variety of landmasses. This paleogeographic history has been invoked to explain aspects of the subcontinent’s modern-day fauna, with a combination of endemic radiations, remnants from Gondwana, and more recent immigrants from Laurasia. Here, network approaches document how vertebrate faunas of the Indian subcontinent, and specifically their relationships to those of other landmasses, changed during the subcontinent’s isolation from close faunal relationships with Madagascar and South America in the Late Cretaceous to a more Laurasian fauna most similar to those of Europe by the Eocene.
AB - The paleogeographic history of the Indian subcontinent is unique among Earth’s landmasses. From being part of the southern supercontinent Gondwana for most of the Mesozoic, through a period of isolation as a drifting entity in the Late Cretaceous, to colliding with Asia near the Paleocene-Eocene boundary, the Indian subcontinent has been associated with, and dissociated from, a variety of landmasses. This paleogeographic history has been invoked to explain aspects of the subcontinent’s modern-day fauna, with a combination of endemic radiations, remnants from Gondwana, and more recent immigrants from Laurasia. Here, network approaches document how vertebrate faunas of the Indian subcontinent, and specifically their relationships to those of other landmasses, changed during the subcontinent’s isolation from close faunal relationships with Madagascar and South America in the Late Cretaceous to a more Laurasian fauna most similar to those of Europe by the Eocene.
KW - Cretaceous
KW - India’s Drift
KW - Vertebrate
KW - Faunal Similarity
KW - Laurasia
KW - Gondwana
U2 - 10.1007/978-3-030-49753-8_9
DO - 10.1007/978-3-030-49753-8_9
M3 - Chapter (peer-reviewed)
SN - 9783030497521
SN - 9783030497552
T3 - Vertebrate Paleobiology and Paleoanthropology
SP - 227
EP - 249
BT - Biological Consequences of Plate Tectonics
A2 - Prasad, Guntupalli V.R.
A2 - Patnaik, Rajeev
PB - Springer
ER -