A KINEMATIC MODEL FOR AFAR DEPRESSION LITHOSPHERIC THINNING AND ITS IMPLICATIONS FOR HOMINID EVOLUTION: AN EXERCISE IN PLATE TECTONIC PALEOANTHROPOLOGY
The plate tectonic model has paleoanthropological implications. Prior to 6.2 Ma the proximal positions of NU-SOM, AR, and the Danakil block suggest sub-aerial conditions prevailed between Yemen and Ethiopia. Uninhibited Africa-Eurasia faunal exchange through Afar and Arabia (corroborated by published geologic and paleontologic data) was tectonically permissible until the time of the earliest hominids. Continued stretching caused the Afar land bridge(s) to disappear during early to mid Pliocene time. Primitive hominid populations living within the Afar Depression became isolated from AR sometime before ~3.2 Ma. With the plateau becoming less habitable due to long term late Neogene cooling, hominids that remained in the Afar Depression were forced to adapt to a much smaller range that was effectively bounded by the already well-developed NU-SOM escarpments and the newly opened Straits of Bab el Mandeb. Increased population pressure exacerbated by potentially severe fluctuations in local climate (well documented by land and marine paleoclimate proxies) may have caused hominids living in Afar to undergo physical and cultural evolution more rapidly and successfully than hominids inhabiting less confined ranges elsewhere in Africa. We suggest that plate tectonic induced isolation caused the Afar Depression to become the cauldron within which our genus homo arose to prominence.
If our interpretation is correct, continental drift played a major role in hominid-to-human evolution.