| Late Miocene ( up to 7 million years ago) | ||
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Phase I: Oreopithecus-like 'Swamp-apes' ancestral to all African great apes arrive in North & East Africa and becomes established in coastal mangrove swamp & gallery forest environment.
Key: Swamp Apes - African Ape / Homo ancestor Dryopithecus / Oreopithecus-like ape. Orang-utan ancestor Pros:
Cons:
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Habitat: This phase of the model is based on the assumption that the earliest apes lived in rather wet habitats dominated by coastal, and probably swampy mangrove forests. Their putative location (what today is the Eastern Mediterranean, north-east Africa and Arabia) underwent dramatic physical changes between 30 and 10 million years ago. Whole coast lines disappeared and re-appeared several times and the Tethys Sea and its derivatives of the region (e.g. the Mediterranean) were alternatively undergoing flooding when reconnected to the oceans and desiccations when they were cut off again. What we now call the Mediterranean was, apparently, flooded and dried up 14 times in the Miocene. Maps Taken from from Dixon et al 2001 Europe 20 mya Europe 10 mya |
Fossil Evidence: Oreopithecus bambolii, a long studied primate that was a putative biped lived around 10 mya in this region (on an island in the Tethys Sea) has been associated with a swamp habitat. Although this 'monkey' is not thought to be part of the Hominoid (ape) line it is interesting to postulate that one of the earliest bipeds may have done so because of the need for wading. See Moyą-Solą et al 1999 for more about fossils of this primate. Various 'Miocene Apes' that lived in less aquatic habitats have been postulated as ancestral to the African apes (including Dryopithecus brancoi) found, at least in one site in "a subtropical, forested, swamp margin environment" Kordos & Begun (2001) but there is a significant gap in the fossil record here. The AHAH model makes the (admittedly rather large) assumption that the species ancestral to the African apes was a climbing-wading ('aquarboreal') swamp ape and that they were already well adapted to mangrove/swamp forests and adopted a climbing/swinging locomotor repertoire in the trees and bipedal wading in water. The model proposes that some of these coastal mangrove apes began to migrate inland, along the rift valley rivers and lakes. It is proposed that Sahelanthropus tchadensis and Orrorin tugenensis the earliest putative bipedal hominids were example of this inward migration possibly on the way to becoming Gorilla. Later, another smaller and more arboreal ape that was more omnivorous - the model proposes - would eventually split from the remaining swamp apes and eventually evolve into the progenitors of Pan and Homo. This model is not prescriptive here about the exact semi-aquatic environment which was responsible for the divergence of the Homo lineage from Pan, but it is proposed that it could have been a combination of coastal mangrove forests and in-land gallery forests, shrinking ever closer to rivers as climate change in East Africa reduced forestation there. |
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Predictions: Specifically:
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Controversions: This phase of the AHAH should be easily controverted if the predictions are overturned or if evidence arises to show that something very different happened. Specifically:
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Phase Ending: It is proposed that phase I of the AHAH model ended after inter-glacial flooding or glacial desiccation occurred causing the vast majority of these putative climbing-wading apes to become extinct. This is a difficulty because the flood/desiccation cycles apparently occurred several times. It is assumed that the last time it happened a group of these climbing-wading apes found themselves in inland forests, forming a radiation of migration of semi-bipedal apes - the Australopithecines.. Those living west of the rift would remain in relatively stable equatorial rain forest habitats, whereas those on the east of the rift would increasingly be exposed to the process of aridification, causing forests to shrink closer to rivers and lakes. That migration and radiation is dealt with in Phase II. |