The dispersal of hominins may have been favored by the opening of the landscape during the Early-Middle Pleistocene transition (EMP) in Western Europe. The structure of the small-vertebrate assemblages of the archaeo-paleontological karstic site of Gran Dolina in Atapuerca (Burgos, Spain) shows important environmental and climatic changes in the faunal succession, across the Matuyama-Brunhes boundary at 780 ka. These changes are interpreted to indicate impoverishment of the forests, along with an increase in dry meadows, and open lands in general that entailed a tendency towards the loss of diversity in small-vertebrate communities above the EMP. We evaluate variation in diversity of the faunal succession of Gran Dolina using Shannon's Second Theorem as an index of ecosystem structure. The long cultural-stratigraphic sequence of Gran Dolina during the EMP is somewhat similar in its completeness and continuity to that in the locality of Gesher Benot Ya'aqov in the Upper Jordan Valley. We also evaluate related data including faunal and floral (pollen) succession. Both localities present cold, dry and humid, warm fluctuations at the transition between the Early and the Middle Pleistocene. Comparisons between these sites present opportunities to understand large-scale climatic changes.
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http://dx.doi.org/10.1016/j.jhevol.2010.04.002 | DOI Listing |
J Hum Evol
December 2021
CENIEH (National Research Center on Human Evolution), Burgos, Spain; Anthropology Department, University College London, London, UK.
The Chinese Middle Pleistocene fossils from Hexian, Xichuan, Yiyuan, and Zhoukoudian have been generally classified as Homo erectus s.s. These hominins share some primitive features with other Homo specimens, but they also display unique cranial and dental traits.
View Article and Find Full Text PDFAnat Rec (Hoboken)
August 2022
Centro Mixto UCM-ISCII de Evolución y Comportamiento Humanos, Madrid, Spain.
Circum-nasal and nasal cavity morphology add to the picture of the Sima de los Huesos specimens as, at one level, representing a distinct morph and, at another, displaying individual variation. They developed a robust, midline-grooved, three-dimensional spinal ridge lying anteriorly in the nasal cavity floor that was distended posteriorly over the nasal cavity floor, and, typically, an expansive, three-dimensional patch of rugose bone on the nasal cavity wall where a conchal crest would otherwise lie. They vary, for example, in degree of topographic relief of the nasal cavity wall, expression of the spinal ridge, and development of nasal crests and fossae.
View Article and Find Full Text PDFJ Anthropol Sci
March 2021
Centro Nacional de Investigación sobre la Evolución Humana, Paseo de la Sierra de Atapuerca 3, 09002, Burgos, Spain; Anthropology Department, University College of London, 14 Taviton Street, London WC1H 0BW, UK.
One of the main concerns of paleoanthropologists is to make a correct interpretation of the variability observed in the fossil record. However, the current knowledge about sexual dimorphism in the human lineage comes mainly from the study of modern human, Neanderthal and pre-Neanderthal populations, whereas information available about the intrapopulation variability of the groups that preceded these taxa is still ambiguous. In this preliminary study, Homo antecessor dental sample was assessed with the aim of trying to evaluate the degree of variability of their permanent canines` dental tissue proportions.
View Article and Find Full Text PDFSci Rep
February 2021
Centro Nacional para el Estudio de la Evolución Humana (CENIEH), Paseo Sierra de Atapuerca 3, 09002, Burgos, Spain.
Two well-preserved, subadult 800 ky scapulae from Gran Dolina belonging to Homo antecessor, provide a unique opportunity to investigate the ontogeny of shoulder morphology in Lower Pleistocene humans. We compared the H. antecessor scapulae with a sample of 98 P.
View Article and Find Full Text PDFJ Hum Evol
August 2020
Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Zona educacional 4, Campus Sescelades URV (Edifici W3), Tarragona 43007, Spain; Dept. d'Història i Historia de l'Art, Universitat Rovira i Virgili (URV), Avinguda de Catalunya 35, Tarragona 43002, Spain; Departamento de Historia, Geografía y Comunicación, Universidad de Burgos, Paseo de los Comendadores s/n, Burgos 09001, Spain.
The Atapuerca localities present evidence of a long series of hominin occupations from the Early Pleistocene onward and are a key site for understanding the continuity and discontinuity of Western European technological and settlement dynamics. The TD10 unit from Gran Dolina is located in the upper part of the sequence and divided into four lithostratigraphic subunits (TD10.4 to TD10.
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