Fossil evidence for seasonal calving and migration of extinct blue antelope (Hippotragus leucophaeus) in southern Africa
Article first published online: 21 JUN 2013
© 2013 John Wiley & Sons Ltd
Journal of Biogeography
Volume 40, Issue 11, pages 2108–2118, November 2013
How to Cite
Tyler Faith, J., Thompson, J. C. (2013), Fossil evidence for seasonal calving and migration of extinct blue antelope (Hippotragus leucophaeus) in southern Africa. Journal of Biogeography, 40: 2108–2118. doi: 10.1111/jbi.12154
- Issue published online: 17 OCT 2013
- Article first published online: 21 JUN 2013
- National Science Foundation Dissertation Improvement. Grant Number: J.T.F. (BCS-0824717)
- Blue antelope;
- Cape Floristic Region;
- extinct species;
- southern Africa;
Palaeoecological data are crucial to understanding the historical extinction of the blue antelope (Hippotragus leucophaeus). This study examined late Quaternary fossil evidence bearing on the blue antelope's calving and migratory habits.
Cape Floristic Region (CFR), South Africa.
Blue antelope mortality patterns were reconstructed from dental remains from fossil assemblages spanning the last c. 200,000 years and located in the CFR's winter and year-round rainfall zones. Two demographic measures were examined: (1) the frequencies of juveniles relative to adults; and (2) the frequencies of neonates relative to older juveniles. Geographical trends were examined across a longitudinal gradient of decreasing winter rainfall and increasing summer rainfall.
There was a significant longitudinal trend in the blue antelope mortality data, with juveniles and neonates declining in frequency from west to east. This suggests that calving occurred primarily in the winter rainfall zone, probably during the winter months when seasonal rains promoted the growth of C3 grasses. The summer drought and lack of adequate forage forced blue antelope to migrate east, in time with summer rainfall and the increased availability of C4 grasses. The migration route probably depended in part on reduced sea levels during glacial phases of the Pleistocene.
Blue antelope were probably migratory. Rising sea levels at the onset of the Holocene disrupted their migration routes, limited access to west-coast calving grounds, and fragmented populations. Such disruption would have devastated the blue antelope population and contributed to its vulnerability to extinction. Blue antelope survived previous marine transgressions, however, suggesting that other factors played a role in its demise. Agricultural expansion early in the colonial era may have further disrupted migration routes and played an important role in its extinction.