Variability and Evolution, 1996, Vol. 5: 29–42 BETINA KUJAWA Institute of Anthropology, Department of Human Population Ecology, Poznan,́ Poland ADAPTIVE ASPECTS OF HOMINISATION: LOCOMOTION, MANIPULATION AND THERMOREGULATION* KUJAWA B. 1996. Adaptive aspects of hominisation: locomotion, manipulation and thermoregulation. Variability and Evolution, Vol. 5: 29–42, Figs. 4, Tab. 1, Adam Mickiewicz University, Faculty of Biology, Poznan´ Abstract. Certain geological, climatic and material traces researched by paleontology allow for the reconstruction of a complex of the adaptive traits that were developed in Australopithecines. Bone remains of the Plio-Pleistocene hominids prove that Australopithecines were undoubtedly erect, bipedal beings, possessing certain advanced manipulative abilities. Information about their physiology (thermoregulation, pigmentation) comes from the comparison between modern man and philogenetically closest anthropoids, or from the specific features of Homo sapiens. Key words: hominids, adaptation, bipedalism, manipulation, thermoregulation, pigmentation „ ... no organism adapts in an abstract way; this phenomenon takes place strictly within specific conditions imposed by the environment.” (Dobzhansky 1983) Introduction Looking at man, or earlier hominid forms, it is difficult to determine the kind of specialisation they represent. The adaptations that characterise anthropoids cannot serve as the basis for comparing them either to strong carnivores, or four-footed ungulates, or quadrupedal savannah baboons. * Paper presented at IV World Archeological Congress in December 1994 in New Delhi. 30 B. Kujawa Since the australopithecine forms evolved in the same environmental conditions as the mammals mentioned before (the African savannah becoming progressively cooler and steppe-like), they could not remain “neutral” in the face of the changing surroundings. Man is unusual among other terrestrial mammals due to his bipedalism, precision of holding and the possession of naked skin. This article provides the most accepted explanation of the evolution of these features which seem to be the adaptations to specific conditions imposed by the environment of the Plio-Pleistocene East Africa. Anatomical aspect Locomotion The very fact of bipedalism, and hence the upright posture, of the Plio-Pleistocene hominids does not raise any doubts or reservations. However, the reason why bipedalism had evolved remains a matter of dispute. Like Darwin (Darwin 1871), many authors try to explain bipedalism in the context of locomotion, and consider the possibility that bipedalism arose as a consequence rather than a cause of the changes relating to the use of the forelimbs. For example Kortland (1980) suggests that bipedalism might have developed as the effect of using the forelimbs for brandishing thorn bush branches in order to scare off attacking carnivores. It seems doubtful, however, that such an action would be sufficient to deter a large carnivore or smaller, pack-hunting animals. In turn Day (1986) claims that the development of bipedal posture and locomotion can be explained in terms of improved survival advantage owing to the more efficient picking of food from high branches, the ability to run and climb trees after an early warning of danger, and having arms free for defending themselves or for safe carrying of infants (considering their prolonged helplessness and dependency). However, it seems more probable that a hominid under threat from a carnivore would have reached the safety of a tree quicker if it made its escape in any other way but bipedal. Moreover, an infant in an adult’s arms is a serious impediment for the carrier both during a flight and while climbing a tree, hence an individual carrying offspring would be more vulnerable than other, even less agile, members of its group. A different view was advanced by Washburn and Howell (1960) who claimed that the use of tools was both the cause and effect of human bipedalism. This hypothesis was further developed but it fell into a pattern of interpreting ’tool use’ as a manipulative and manufacturing activity. Meanwhile, the available reports on protocultural behaviour patterns of many higher primates have proven that the customary posture during manipulative activity is the sitting posture, a fact which contradicts the hypothesis about a significant contribution of such behaviour to the development of the upright posture or bipedalism. Adaptive aspects of hominisation 31 Thus, the most important problem, namely, why the Plio-Pleistocene hominids became bipedal while the related forms remained arboreal, vertical climbing animals, remains unsolved. An interesting proposition for solving this question, supported by appealing arguments, is the so called “throwing hypothesis” put forward by Fifer (1987). This hypothesis proposes that both the fore- and hind limbs of man were, and still are, integral parts of a single functional mechanism, hence the main evolutionary driving force of human bipedalism was the development of a muscular system which would be efficient and effective during “missile-launching”. This mechanism, activating the morphology and anatomy of the whole body, explains the development of many specific structural features of the lower half of the skeletal and muscular systems in a manner superior to the mechanism of bipedal locomotion itself. According to Fifer’s concept (1987), the factor which initiated the separation of evolutionary lines of the hominids and chimpanzees from a common ancestor was, as the author proposes, behavioural in its nature with “(...) the protohominid preferring to stand its ground and hurl stones at the attacker and with the proto-chimpanzee preferring to threaten by brandishing branches (a threat backed by powerful jaws and large canine teeth) and, if this failed, to take to its heels and make a fast get-away to the nearest tree – on all fours of course” (1987, p. 139). The regions of East Africa had been separated by a developing system of rifts, thus isolating two populations of hominids which thereafter evolved in different environmental conditions (Okołowicz 1969; Ksia˛żkiewicz 1979; Foster 1983; Andel 1985; Coppens 1989). It appears, therefore, that it was the environment that created the behavioural preference suggested by Fifer. The use of stones, being as it were “at hand”, might have created such behavioural preference in a group of hominids because of its effectiveness, and subsequently this preference would be incorporated into the range of behavioural patterns of the group. Natural selection, in turn, would favour those individuals who were better adapted to the action of missile launching. The anatomical features which developed at that time are also characteristic of modern man, and the specific as well as atypical nature of these features seems to be explainable precisely by Fifer’s “throwing hypothesis”. The author himself calls these features “anomalies” and attempts to justify their existence by an evolutionary pressure in the times of the Plio-Pleistocene to perfect the mechanics of a throw. Fifer (1987) includes the following among these features: (Fig. 1) – massiveness of the lower limbs in relation to the upper parts of the body, a feature that impedes rapid acceleration but enables a greater speed of upper limbs movement necessary for effective stone throwing, – a strongly developed largest gluteal muscle (musculus gluteus maximum) which performs most effectively when the knee joint is fully extended, and the least in the walking gait, a muscle which takes the role of a “stabiliser” or counterbalance when a stone is thrown forward and causes the thrower to lose his 32 B. Kujawa Fig. 1. Morphological (long and mobile torso, double-spiral arrangement of the body musculature) and anatomical (muscles) features which perfect the mechanics of a throw balance, a relatively long and mobile torso which, in order to maintain a stable posture during walking or running, requires the activated muscles to outlay additional energy, but which makes the missile-launching mechanism more effective through a “doublespiral arrangement” of the human body musculature as described by Dart (1950). The “stone throwing” hypothesis is very interesting and it contributes new elements to the anthropogenetic debate, although it does not take into consideration other important features of the human anatomy, features whose presence suggests in an obvious way a strong selection favouring individuals better adapted to bipedal walking. The discussion presented above confirms that Australopithecines commonly used large stones, at least in defence or attack. However, because of the canines size reduction, gathering and processing vegetable food as well as fragmenting captured or found animals required of Australopithecines the ability to use stones for tools with precision. 33 Adaptive aspects of hominisation Manipulation Evidence supporting the thesis that the Plio-Pleistocene Australopithecines used stone tools (and possibly made them) can be found in the anatomy of these creatures which, after all (besides appropriate nervous centres), determines the manipulative abilities of the hand. As it turns out, the structure of distal phalanges in the primate hand is considered to be one of the crucial factors enabling precision holding. According to Shrewsbury (1986, p. 234), precision holding can be defined as “combinations of the proximal or distal ungual pulp of the pollex, or its non-pulp surface, in apposition to the proximal or distal ungual pulp of another digit(s), or its non-pulp surface(s), for the purposes of differential prehension.” According to Johanson (1982), the structural differentiation of the ungual pulp into proximal and distal regions occurs only in humans. This structural differentiation determines certain contrasting functional properties of two areas as shown in Table 1. Table 1 Comparison of the functional properties of the ungual pulp in Humans Property sensory area Proximal area larger Distal area smaller tactile discrimination higher lower friction ridges longitudinal lateral mobility greater lesser The structural and functional differentiation of the ungual pulp regions enables performing several clearly distinct varieties of precision holding which have been called „types” and have been given numbers from I to IV (Fig. 2). Comparative analysis of the distal phalanx structure in primates has shown that the functional differentiation (compartmentalisation) of the human ungual pulp is determined by a different shape of the phalanx. In the human hand the distal phalanx is ended in a significantly broadened ungual tuft with a rough volar surface (Shrewsbury 1986), or in other words, ungual tuberosity (Bochenek 1992). In apes this part of the phalanx is shaped into an obtuse cone with a smooth volar aspect (Fig. 3). This explains the absence of radially extending ligaments in apes which in man are attached precisely to that rough tuberosity (Aiello 1990). Further, the distal phalanx in man reveals spiny bone structures to which intraosseous ligaments are attached from the sides, restraining and supporting the proximal part of the ungual pulp. Similar structures are not encountered in other primates. For reasons presented above, the ungual pulp in apes does not exhibit diverse (regional) mobility and deformability. What were the manipulative abilities of early hominids? 34 B. Kujawa Fig. 2. Four types of precision holding are represented for the human hand The studies included well preserved distal phalanges of the Plio-Pleistocene hominids: two specimens from Hadar, representing the species Australopithecus afarensis, one specimen from Kromdraai of the species Australopithecus robustus, two from Olduvai, ascribed to the species Homo habilis. It is worth recalling that one of the major features of the human hand is the broadened, rugged ungual tuft, unique among primates. It turns out that the development of this feature of the distal phalanx in the Plio-Pleistocene Australopithecines varies. The early Hadar forms (dated at 2.9–3.3 million years), according to Stern and Susman (1983), exhibited only a moderate lateral broadening of the distal Fig. 3. Palmar view of the distal phalanx of a human and a chimpanzee. Note the area of insertion for flexor pollicis longus on the human bone Adaptive aspects of hominisation 35 phalanx, comparable with a smooth, conical ending of the phalanx in pongids. On the other hand, the ungual tuft in the Olduvai forms (dated at 1.8 million years) is already finally developed and comparable to that of the Homo sapiens. It supports the view that the Hadar Australopithecines were capable of types I, II and III precision holding, and the Olduvai forms additionally, though still imperfectly, of type IV precision grip. Hence, the morphology of their phalanges can be defined as “transitional” between the ape and human forms. In particular the early, Pliocen, hominids, even though already bipedal, partially exhibited the traits of arboreal creatures in the way that their forelimbs had not yet been completely released from the locomotor functions. Hence, their manipulative abilities could not have developed to the same extent as in later forms. It has to be presumed that the appearance of first stone tools coincided with the development of ungual tuberosity. It would confirm the early productive activity of Australopithecines, an activity the development of which could only be successful in specific terrain conditions. This is because the materials used for tools, or their prototypes, do not occur with equal frequency in different areas of the African continent. Stones with sharp edges can be found most readily in the middle and upper sections of rapid-flowing rivers, or in volcanic terrain. Basalt and flint, occurring in abundance in the latter areas (and incidentally the oldest tool-making material), are, due to their structure, perfect for secondary processing. No wonder, then, that the populations of Australopithecines showed such a preference for the volcanic plateau of East Africa. Physiological aspect Thermoregulation The East African Plateau was exceptionally favourable to the Australopithecines for another reason. The Plateau, because of its equatorial position, enjoyed intensive sunshine which undoubtedly led to the evaporation of many shallow lakes, leaving strongly saline water at the bottom. Additionally, owing to a strong volcanic activity, the region abounded in volcanic ashes, rich in minerals. The tectonic activity connected with the formation of the East African Rift created favourable conditions for the emergence of shallow salt lakes. Water was not in short supply in this region either. The rainy season provided even surplus water, while in the dry season at least several rivers flowing from the mountains supplied adequate amount of water. Of course those water sources were not (and still are not) distributed evenly over the whole area of the East African Plateau, but they were reasonably close to each other to enable ready use of those sources during the dry season (Newman 1970; Weiss 1981; Tobias 1991). 36 B. Kujawa The environmental conditions described above turned out to be necessary for the evolution of certain physiological mechanisms in the early hominids, traits which facilitated their survival in the savannah environment of the African tropics. It seems that the biggest problem faced by mammals living in the tropics is the dissipation of body heat, since overheating of the organism is inevitably fatal (Szarski 1990). There are many ways to cope with the surplus heat generated by the body or absorbed from the external environment (Schmidt-Nielsen 1983). It may be an increased blood flow through the almost hairless skin of external ears (auricles), or antlers, or the cooling of venous blood through evaporation of water from the mucous membrane of the nasal cavity and sinuses in certain parts of the cranium (thus the blood is cooled before it flows to the cranium, a fact which allows maintaining brain temperature at several degrees lower than the temperature of blood in the arteries of neck and trunk). It can also be achieved by way of cooling of the nasal cavity, fauces and tongue through rapid shallow inhalations (Szarski 1990). In the case of the Hominidae family it appears that the adaptive response to unfavourable tropical savannah conditions included, simultaneously, several morphological and physiological aspects of the organism, forming together an integrated functional system. This system, covering hair reduction, eccrine sweat glands, and dark-pigmented skin probably evolved concurrently with bipedal locomotion (Zihlman 1988). These morphological and physiological adaptations can be explained in the context of specific ecological conditions of the Plio-Pleistocene East Africa. An intensive insolation of the open equatorial terrains during the day created completely different climatic conditions from those prevailing in a humid tropical forest. Excluding the periods of intensive rain, the tropical forest maintains the near-ground temperature of about 28–32oC, which accompanied by slow air movement, high humidity and reduced sunshine creates conditions in which heat dissipation from the organism is not a major problem. In the open savannah an individual is exposed to direct solar radiation and additionally absorbs heat radiating from nearby objects. Any physical activity (and with Australopithecines such activity was probably increased due to the dispersal of water sources and food) requires additional energy outlay, hence the amount of body heat increases, in this case generated by the working muscles. Even moderate physical effort doubles the Basal Metabolic Rate (Zihlman 1988). Such combination of external and internal (organic) heat, if not dissipated, would dangerously raise the temperature of the brain, leading to death. It appears, however, that Morgan was not right when she claimed that the evolution of the upright posture and bipedal locomotion ought to be explained by a smaller surface area of the body exposed to solar radiation and to easier loss of body heat compared to a horizontal posture of quadrupeds (Fig. 4) (Morgan 1982). The energy cost of maintaining such a posture was, after all, high, and this fact was not compensated for by any solution to the problems connected with excess body heat. Adaptive aspects of hominisation 37 Fig. 4. Estimates of the total body surface area exposed to direct solar radiation by a hominid, in bipedal and quadrupedal position, as a function of solar elevation According to Schmidt-Nielsen (1983), similarly to other savannah animals (particularly ungulates), the system of draining venous blood from the scull in man has been “designed” to cool the brain under conditions of hypothermia. Changes in air temperatures induce changes in the tension of the smooth muscles of facial blood vessels, and that in turn changes the direction of venous blood drainage in the skull. The venous blood thus flows from the face through the ophthalmic veins and their astomoses down the skull, so that the arterial blood can dissipate heat in the cavernous sinuses and, cooled, proceed to the brain (Schmidt-Nielsen 1983). A very important role in this cooling mechanism is played by the nasal cavity which houses a system of arteriovenous vascular plexus, facilitating efficient heat and moisture exchange. As Beals (1986) suggests, the evolution of this vascular system of thermoregulation could cause changes in the shape of the base of the skull. Conroy (1980) observed the relation between the patterns of cerebral veins reticulation and the sizes and shapes of openings in the base of the skull. It is important because there is ample evidence that the size and shape of the base of the skull determines the shape of the cranial vault and face (Beals 1986). Perharps further research could prove that the expansion of cavernous sinuses and the increased amount of cranial fluid, which led to a greater volume of craniums and caused their transformation, was a “prelude” to the expansion of the brain during subsequent 38 B. Kujawa stages of evolution. Close to that view is Fiałkowski’s hypothesis (Fiałkowski 1978; Bielicki 1987) about the increasing volume of the Plio-Pleistocene hominid brains being an adaptation of this organ to a reliable functioning under the hypothermia of the body due to a great physical effort during “endurance hunting”. A strong heat shock put the functioning of cortical neurons at risk, which would be fatal to an individual. As Fiałkowski claims, the adaptation to that stress could lie in the creation of additional cortical neurons and an additional number of connections between them: then the brain as a whole would function properly even if some of the neurons were momentarily blocked. It seems doubtful, however, that this hypothesis is correct if we consider that the brain is metabolically a very costly organ. According to Amstrong (1983), the brain, representing about 2 percent of the total body mass, continuously uses nearly 20 percent of the body’s energy (Beals 1986). It is difficult to see that an organ consuming so huge amounts of energy could passively increase its size by way of natural selection. It has to be noted that the first distinct changes in the intracranial vascularisation appear on the casts of the craniums of the Plio-Pleistocene Australopithecines (Zihlman 1988; Coppens 1991). The cranial thermoregulatory system was not sufficient to dissipate large surpluses of body heat. As we mentioned before, a whole system of adaptive features of the skin evolved, a system that enabled the survival and efficient functioning of the hominids subjected to the stress inducting heat conditions of the savannah. In humans the skin is an organ participating in the mechanisms responsible for dissipating excess body heat, hence, no doubt, it also played a significant role in the early hominids. One method of stabilising the outflow of heat from the body was the initiation of the surface blood flow. When blood vessels in the skin dilate the warmer blood from inside the body flows to the skin surface raising its temperature and thus enabling heat loss through conduction, convection (the physical phenomenon whereby the warmer air moves up and the cooler air – down) and radiation. In this context important becomes the fact that the large muscles fulfilling the locomotor function are located not on the torso but on the legs (the thigh and shin), hence the heat generated by these muscles only to a limited extent ends up in the circulatory system. As Reichholf notes, such “structural design” obviously prevents excessive, and dangerous, overheating of the body (Reichholf 1990). The high efficiency of thermoregulatory processes, however, is only possible thanks to a large number of eccrine sweat glands (about 2 million) distributed over the whole surface of the body. They produce sweat which is carried to the skin surface through ducts opening in the skin pores. Evaporation of sweat in higher temperatures can lead to a loss of up to 2 litres of water in one hour, with every gram of evaporated water dissipating 0.56 cal of heat energy (Zihlman 1988). Such a mechanism of heat regulation requires the supply of adequate amounts of water and salt in order to compensate for the losses incurred in sweating. As the Adaptive aspects of hominisation 39 topographic description of the African Plateau shows, during the evolution of the skin thermoregulatory mechanisms this condition was satisfied. At the same time the evolution of hormonal control mechanisms took place, mechanisms which limited the loss of elements valuable to the organism through the secretion of such hormones as the antidiuretic hormone (ADH) causing secondary absorption of water from primary urine, or aldosterone which increases the reabsorption of sodium ions in kidneys and eccrine glands. Despite earlier results obtained by Montagna (1963), a research carried out by Johnson (1974) in the late nineteen seventies on perspiration in primates has shown that a loss of heat in the process of evaporation occurs in certain species of baboons, rhesus monkeys and macaques, albeit to a much lesser extent than in man. In this process the eccrine glands are engaged which prevail over the apocrine glands in these primates. The closest to man in respect of the amount of sweat secretion are savannah red talapoins (Erythrocebus patas). They sweat in particular after an intensive run in high temperatures, but also during a rest, which explains their increased tolerance to heat compared with forest primates. Compared with rhesus monkeys they sweat 2 to 6 times more profusely and their eccrine glands are also distinctly larger (Zihlman 1988). The primates inhabiting savannah areas are also more dependent on water sources (Newman 1970). The above data shows that the development of an efficient thermoregulatory system played a decisive role in survival and efficient functioning in the conditions of the tropical savannah. The similarities of evaporation process involving numerous eccrine glands in the hominids and savannah talapoins highlights to an even greater extent the role of the environment in the development of appropriate adaptive mechanisms. In the early hominids, however, the functioning of eccrine sweat glands was further enhanced through the loss of hair (in the sense of reduction of the length and thickness of hair). As Amaral (1989) suggests, body hair performed numerous, important to a hominid, functions: heat retention in low temperatures at night, protection against harmful solar radiation, shock absorption of falls and hits, protection against sharp fangs or claws of attacking animals, establishing hierarchy by way of hair bristling, enabling an infant or a growing child to cling to its mother. The losses due to hair reduction must have been smaller than the gained advantages. The only explanation of the hair loss phenomenon is the increased effectiveness of human thermoregulation through the loss of heat during sweat evaporation. Naked skin allows the overheated body to dissipate heat quickly, whereas thick body hair retains heat through an insulating layer of trapped air. The amount of body hair among different human populations varies, nevertheless in all humans the skin surface is sufficiently exposed to permit efficient dissipation of heat by perspiration. Still, the hair on the head has been retained, as well as in the armpit areas and around external genitals. The retention of hair on the head is 40 B. Kujawa probably important for the protection of this part of the body (containing the brain) against short wave ultraviolet radiation, and the role of hair in temperature regulation of this organ (be it during a sunny day or cold night) – a regulation necessary because of the absence of protective layer of muscles or subcutaneous fat. The pubic and axillary hair in humans is, firstly, a sign of sexual maturity (conditioned, incidentally, by hormones), and secondly, a place for the sustentation of sexual (maybe attracting?) aromatic substances. Pigmentation Beside visible light and long-wave (infrared) thermal radiation, the solar spectrum contains also ultraviolet radiation. The described perspiration mechanism does not protect the body against harmful effects of the latter, such as sunburn of the skin with blisters, liable to cause infection. For as long as the skin was protected by a thick coat of hair, as in other African apes, the danger of direct ultraviolet radiation was small. Thus, during the phase of hair reduction a conflict must have arisen, caused by pressure factors working towards slowing the process down, unless at the same time another adaptive trait had emerged which reduced the harmful effect of that part of the solar spectrum. It appears that such a defensive mechanism was provided in dark pigmentation of the skin. The skin colour among the living human populations varies depending on the amount of pigment (melanin) in the epidermis. The melanin production is stimulated by solar radiation, and the produced pigment in turn absorbs the ultraviolet portion of the solar radiation, thus neutralising the harmful effect. The hairy skin of other primates is diverse in colour: even the same specimen can have a differently and irregularly pigmented body. It is, therefore, unlikely that the skin colour can play any role in their survival. Then, as Zihlman (1988, p. 399) states: “the dark-pigmented skin played a significant, even decisive, role in survival, therefore it became a common feature among the early hominids.” Since the skin pigmentation in African apes is highly diversified, it is most likely that the populations of hominids emerging in the Pliocene was also diverse in respect of this feature. Presumably, then, the hair reduction phase coincided with the selection of dark-pigmented skin. The protective function of dark skin in the environment where ultraviolet radiation is most intense and prolonged must have played a role in the differentiation of survival advantage and reproductive success of hominids (Zihlman 1988). A question remains, however, of the already mentioned diverse amount of melanin in the skins of the present-day humans inhabiting the whole area of the Earth. The only advantage of the light skin over dark is that an individual having a lighter skin complexion is able to produce more vitamin D (calciferol) from a unit of radiation. Taking this into account, one can wonder about a potential regress in the selection of dark-pigmented skin, the more so that in the Plio-Pleistocene environment of African savannah the food sources rich in calciferol were probably scarce Adaptive aspects of hominisation 41 (fish, egg yolk, milk). Assuming, however, that Australopithecines were exposed to prolonged ultraviolet radiation, they probably were able to produce sufficient amounts of this vitamin, even though their skins were darker. Then, the lighter skin is in modern times characteristic of the populations inhabiting high latitude areas, thus it would compensate for the lower intensity of ultraviolet radiation and possible vitamin deficiency in the diet. Conclusion The evolution of the family of Hominidae is connected with the great geological and climatic events that happened in the late Miocene. The reactivation of the East African Rift and its consequences, as for instance the cooling of climate and the drying of the south-eastern parts of Africa where Australopithecines were exposed to the adaptive radiation, determined the direction of the changes that affected the earliest human forms. The changes were of tree kinds: morphological, physiological and behavioural. The sudden retreat of tropical forests and the expansion of open savannah resulted in the conditions that required a specific adaptation. Australopithecines made many attempts to face the conditions and realise the process of adaptation. Undoubtedly, the most advantageous appeared: bipedality (which arose from the development of a defence mechanism – throwing of stones), manipulatory skills (precise holding but not as fully perfected as it is in contemporary humans), the effective thermoregulatory system (eccrine sweat glands, reduction of body hair, dark skin pigmentation). Probably the evolving adaptive traits were strictly connected with one another. This kind of connection is called the positive feedback loop. References Aiello L., Ch. Dean 1990. An introduction to human evolutionary anatomy. Academic Press, London. Amaral do L. Q. 1989. Early hominid physical evolution. Human Evolution 4: 33–44. Amstrong E. 1983. Relative brain size and metabolism in mammals. Science 220: 1302–1304. Andel van T. H. 1985. New views on an old planet. Continental drift and the history of the Earth. Cambridge University Press, England. Beals K. L. 1986. Brain Size, Cranial Morphology, Climate and Time Machines. Current Anthropology 25: 301–330. Bielicki T. 1987. Evolution of hominids’ brain. Kosmos 36: 545–562 (in Polish). Bochenek A. 1992. Human anatomy. vol. I, PZWL, Warszawa (in Polish). Conroy G. C. 1980. Cerebral venous hemodynamics and basicranium of Cebus. American Journal of Physical Anthropology 53: 37–42. Coppens Y. 1989. Les Hominides du Pliocene et du Pleistocene d’Afrique Oriental et leur environnement. La vie de Sciences 5: 156–168. 42 B. Kujawa Coppens Y. 1991. L’evolution de hominides, de leur locomotion et de leur environnement. Cahiers de Paleoanthropologie 296–299. CNRS, Paris. Day M. H. 1986. Bipedalism: pressures, origins and modes. In: Major topics in primate and human evolution (ed.) Wood B., Lawrence M., Andrews P. Cambridge University Press. Dart R. A. 1950. Voluntary muscle in the human body. The double spiral arrangement. British Journal of Physical Medicine 13: 265–268. Darwin C. 1871. The descent of man. (2nd Edition, 1913) Murray, London. Dobzhansky T. 1983. Human Culture. A moment in Evolution. Columbia University Press, New York. Fiałkowski K. 1978. Evolution of hominid brain. Studies in Physical Anthropology 4: 56–78. Fifer F. C. 1987. Adoption of bipedalism by hominids – a new hypothesis. Human Evolution 2: 135–147. Foster R. F. 1983. General geology. Colombus, Toronto. Johanson D. C., M. Taieb, Y. Coppens 1982. Pliocene hominids from the Hadar Formation, Ethiopia: stratigraphic, chronological, and peleoenvironmental contexts, with notes on hominid morphology and systematics. American Journal of Physical Anthropology 57: 373–402. Johnson G. S. 1974. Eccrine sweat gland in Macaca mulatta. Journal of Applied Physiology 37: 814–820. Kortland E. 1980. How might early hominids have defended themselves against large predators and food competitors. Journal of Human Evolution 9: 79–112. Ksia˛żkiewicz M. 1979. Dynamical Geology. PWN, Warszawa (in Polish). Montagna W., J. S. Yun 1963. The Skin of Primates. American Journal of Physical Anthropology 21: 189–204. Morgan E. 1982. The aquatic ape. A theory of human evolution. Stain and Day, New York. Napier J. R. 1962. Fossil hand bones from Olduvai Gorge. Nature 196: 409–411. Newman W. 1970. Why Man is sweaty and thirsty naked animal? Human Biology 42/2: 126–134. Okołowicz W., 1969, General Climatology. PWN, Warszawa (in Polish). Reichholf J. H. 1990. Das Ratsel der Menschwerdung – Die Entstehung des Menschen im Wechselspiel mit der Natur. Deutscher Taschenbuch Verlag GmbH & Co. Kg, München. Schmidt-Nielsen K. 1983. Animal physiology: Adaptation and environment. Cambridge University Press, England. Shrewsbury M. M., A. Sonek 1986. Precision holding in humans, non-human primates and Plio-Pleistocene hominids. Human Evolution 1: 233–242. Stern J. T., R. L. Susman 1983. The locomotor anatomy of Australopithecus afarensis. American Journal of Physical Anthropology 60: 279–317. Szarski H. 1990. Vertebrates’ story. PWN, Warszawa (in Polish). Tobias P. V. 1991. The environmental background of hominid emergence and the appearance of the genus Homo. Human Evolution 6: 129–141. Washburn S. L., F. C. Howell 1960. Human evolution and culture. In: Evolution after Darwin (ed.) E. Tax. Chicago University Press. Chicago. Weiss M. L. 1981. Human biology and behavior on anthropological perspective. Academic Press, Boston. Wheeler P. 1984. The Evolution of Bipedality and Loss of Functional Body Hair in Hominids. Journal of Human Evolution 13: 91–98. Zihlman A. L., B. A. Cohn 1988. The adaptive response of human skin to the savannah. Human Evolution 3: 397–409.
© Copyright 2026 Paperzz