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Pachyostosis & pachyosteosclerosis
Of the genus Homo, Homo erectus fossils are those which consist of abnormally thick, heavy, mineral rich bones, especially in the cranium and leg bones. This can only be explained as a clear adaptation towards a shallow diving lifestyle and in no way towards a life of running across the savannah. Until now, there have been few theories put forward to suggest why Homo erectus' bones were so thick and heavy. (Above: manatee and dugong skeletons showing thick, heavy bones for diving / ballast). Pachyosteosclerosis in Archaic Homo: Heavy Skulls for Diving, Heavy Legs for Wading?Stephen Munro and Marc Verhaegen[1]AbstractCompared to the skeletons of all other primates, including Homo sapiens, the crania and postcrania of Homo erectus were typically massive, displaying extremely thick bones with compact cortices and narrow medullary canals. Even outside the primate order, examples of animals displaying such massive bones are rare. Although this feature is sometimes seen as diagnostic of H. erectus, few convincing hypotheses have been put forward to explain its functional and adaptive significance.
Original fossils of Pithecanthropus erectus (now Homo erectus) found in Java in 1891. [1] Stephen Munro and Marc Verhaegen, Pachyosteosclerosis in Archaic Homo, Chapter 5. Was Man More Aquatic in the Past? Fifty Years after Alister Hardy, Waterside Hypotheses of Human Evolution, Bantham science publishers, 2011. p. 82 - 105. "Pachyostosis" in aquatic amniotes: a review.Abstract During the course of amniote evolution, numerous taxa secondarily adapted to an aquatic life. It appears that many of these taxa primitively display "pachyostosis," an osseous specialization characterized by an increase in bone compactness and/or volume. The term "pachyostosis" is used in morphological and histological descriptions to describe what in fact corresponds to different patterns. The aim of this paper is to present the current state of knowledge relative to this adaptation among aquatic amniotes. All the taxa that have returned to an aquatic environment are listed. Moreover, their degree of adaptation to the marine environment, their life environment, and the nature of their "pachyostotic" pattern, when present, are described. This inventory enables the evaluation of the current quality of the data relative to this specialization and provides an indication of the work that remains to be done. The functional consequences of "pachyostosis," and notably its importance for buoyancy control in the context of hydrostatic regulation of the body trim, are discussed and opposed to the requirement of improved swimming abilities in the case of a hydrodynamic mode of trim regulation. Questions are posed about the signification of the polymorphism displayed by this specialization between different taxa, different specimens of the same taxon and different bones of the same specimen, and the problem of quantification of pachyostosis is discussed. © 2009 ISZS, Blackwell Publishing and IOZ/CAS. http://www.ncbi.nlm.nih.gov/pubmed/21392306 Full paper: http://onlinelibrary.wiley.com/doi/10.1111/j.1749-4877.2009.00146.x/pdf Correlation of Bone Density in Aquatic and Semiaquatic Animals to Ecological and Dietary SpecializationsSulman JR, Madelyn GC, Irina AK 2020 One of the most obvious adaptations of animals re-introduced to an aquatic environment is the difference in bone density. Numerous marine mammals & marine reptiles exhibit changes in bone density that correlate to their habitat (ecological niche) & dietary specializations, not phylogenetic relationships. Increased bone density (either pachyostosis, osteosclerosis, or pachyosteosclerosis) was observed early in the transition of terrestrial taxa to the aquatic environment. Animals such as early cetaceans & sirenians clearly exhibit these adaptive features, and even retain many terrestrial characters such as hind limbs & behaviors such as paddle swimming. The increase in bone density is a more energetically efficient hydrostatic mechanism for buoyancy for marine mammals with large lung volumes. As the taxa became more specialized for the aquatic environment morphologically (evolving fins, flippers & flukes) & behaviorally (evolving an oscillating swimming mechanism), variation in bone density correlates with their ecological niche: Modern sirenians retain increased bone density, allowing these large-sized mammals to remain submerged in shallow waters, to feed on sessile littoral foods (sea grasses). The bone density in modern cetaceans became more osteoporotic, allowing them to swim faster, and hunt faster moving prey. Pinnipeds live in a wide range of habitats (from cold to warm waters) and demonstrate varying feeding mechanisms, ranging from filter feeding on krill, bottom feeding on mollusks, and/or catching fast moving prey. Bone density is one vital character that can be used to predict the specific ecological niche & feeding preference for pinnipeds. Some early hominids have been shown to have an increase in bone density. These heavier, thicker bones would make it easier for early Homo to hunt in waters for littoral food sources, and would compensate for the lack of stability from bipedalism. "Evolution of Sirenian Pachyosteosclerosis, a Model-case for the Study of Bone Structure in Aquatic Tetrapods"V de Buffrénil cs 2010 Journal of Mammalian Evolution 17:101-120 Osteosclerosis (inner bone compaction) & pachyostosis (outer hyperplasy) of bone cortices (swollen bones) are typical features of tetrapods secondarily adapted to life in water. These peculiarities are spectacularly exemplified by the ribs of extant & extinct Sirenia. Sea-cows are thus the best model for studying this kind of bone structural specializations. The ribs of 15 spp (from the most basal form Pezosiren portelli up to extant taxa) were studied, and compared to other mammalian spp from both morphometric and histological points of view. Pachyostosis was the first of these 2 specializations to occur (mid-Eocene) and is a basal feature of the Sirenia. But it subsequently regressed in some taxa that do not exhibit hyperplasic rib cortices. Osteosclerosis was only incipient in P.portelli. Its full development occurred later, end-Eocene. These 2 structural specializations of bone are variably pronounced in extinct & extant sirenians, rel.independent from each other, although frequently associated. They are possibly due to similar heterochronic mechanisms bearing on the timing of osteoblast activity. These results are discussed with respect to the functional constraints of locomotion in water. |
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