32 research outputs found

    Messinian age and savannah environment of the possible hominin Graecopithecus from Europe

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    Dating fossil hominids and reconstructing their environments is critically important for understanding human evolution. Here we date the potentially oldest hominin, Graecopithecus freybergi from Europe and constrain the environmental conditions under which it thrived. For the Graecopithecus-bearing Pikermi Formation of Attica/Greece, a saline aeolian dust deposit of North African (Sahara) provenance, we obtain an age of 7.37-7.11 Ma, which is coeval with a dramatic cooling in the Mediterranean region at the Tortonian-Messinian transition. Palaeobotanic proxies demonstrate C4-grass dominated wooded grassland-to-woodland habitats of a savannah biome for the Pikermi Formation. Faunal turnover at the Tortonian-Messinian transition led to the spread of new mammalian taxa along with Graecopithecus into Europe. The type mandible of G. freybergi from Pyrgos (7.175 Ma) and the single tooth (7.24 Ma) from Azmaka (Bulgaria) represent the first hominids of Messinian age from continental Europe. Our results suggest that major splits in the hominid family occurred outside Africa

    Earliest evidence of caries lesion in hominids reveal sugar-rich diet for a Middle Miocene dryopithecine from Europe.

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    The formation of dental caries is mainly caused by dietary habits and therefore, may contain information for dietary reconstructions of fossil hominids. This study investigates the caries lesion in the 12.5 Ma old type specimen of Dryopithecus carinthiacus Mottl 1957 (Primates, Hominidae) from St. Stefan (Austria). Potential food sources are identified on associated palynological data, which allow conclusions about food quality, sugar availability and the hominid metabolism during the Middle Miocene. Using micro computed tomography (μCT) and scanning electron microscopy (SEM) we provide a detailed analysis and characterization of the individuals' caries type. Its lesion is compared with a dataset of 311 wild chimpanzees, indicating morphological and etiological differences in caries formation between both species. The affected molar of D. carinthiacus reveals features known from severe dental caries in humans: (1) Cavitation with steep walls and smooth surface; (2) Reparative dentine at the roof of the pulp chamber; (3) Sclerotic dentine below the cavitation; (4) Association with dental calculus and (5) Unilateral usage of the healthy right tooth row. Its advanced primary caries, initiating on the intact enamel surface, indicates a frequent intake of highly cariogenic sugar-rich fruits, which likely exceeds the frugivory of extant chimpanzees. This finding corresponds with the associated palynological record, which infers a habitat with nearly year-round supply (9-10 months/year) of high quality foods (>carbohydrates; < fibers). Our conclusions challenge the model of a step-wise increase in dietary quality during hominid evolution and support the uricase hypothesis, which discusses the hominid autapomorphy of a fructose-based fat accumulation for periods of starvation. This model receives further validation by the identification of soft-tissue preservation, interpreted as fossilized white adipose cells, in the articulated hominid skeleton of Oreopithecus bamboli from Italy

    Pitfalls in HTTP Traffic Measurements and Analysis

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    Abstract. Being responsible for more than half of the total traffic volume in the Internet, HTTP is a popular subject for traffic analysis. From our experiences with HTTP traffic analysis we identified a number of pitfalls which can render a carefully executed study flawed. Often these pitfalls can be avoided easily. Based on passive traffic measurements of 20.000 European residential broadband customers, we quantify the potential error of three issues: Non-consideration of persistent or pipelined HTTP requests, mismatches between the Content-Type header field and the actual content, and mismatches between the Content-Length header and the actual transmitted volume. We find that 60 % (30 %) of all HTTP requests (bytes) are persistent (i. e., not the first in a TCP connection) and 4 % are pipelined. Moreover, we observe a Content-Type mismatch for 35 % of the total HTTP volume. In terms of Content-Length accuracy our data shows a factor of at least 3.2 more bytes reported in the HTTP header than actually transferred.

    Investigating IPv6 Traffic - What Happened at the World IPv6 Day

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    Abstract. While the IETF standardized IPv6 more than fifteen years ago, IPv4 is still the prevalent Internet protocol today. On June 8th, 2011, several large content and service providers coordinated a large-scale IPv6 test-run, by enabling support for IPv6 simultaneously: the World IPv6 Day. In this paper, we compare IPv6 activity before, during, and after the event. We examine traffic traces recorded at a large European Internet Exchange Point (IXP) and on the campus of a major US university; analyzing volume, application mix, and the use of tunneling protocols for transporting IPv6 packets. For the exchange point we find that native IPv6 traffic almost doubled during the World IPv6 Day while changes in tunneled traffic were limited. At the university, IPv6 traffic increased from 3–6 GB/day to over 130 GB/day during the World IPv6 Day, accompanied by a significant shift in the application and HTTP destination mix. Our results also show that a significant number of participants at the World IPv6 Day kept their IPv6 support online even after the test period ended, suggesting that they did not encounter any significant problems.

    Neogene hyperaridity in Arabia drove the directions of mammalian dispersal between Africa and Eurasia

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    The evolution of the present-day African savannah fauna has been substantially influenced by the dispersal of Eurasian ancestors into Africa. The ancestors evolved endemically, together with the autochthonous taxa, into extant Afrotropical clades during the last 5 million years. However, it is unclear why Eurasian ancestors moved into Africa. Here we use sedimentological observations and soluble salt geochemical analyses of samples from a sedimentary sequence in Western Iran to develop a 10-million-year long proxy record of Arabian climate. We identify transient periods of Arabian hyperaridity centred 8.75, 7.78, 7.50 and 6.25 million years ago, out-of-phase with Northern African aridity. We propose that this relationship promoted unidirectional mammalian dispersals into Africa. This was followed by a sustained hyperarid period between 5.6 and 3.3 million years ago which impeded dispersals and allowed African mammalian faunas to endemically diversify into present-day clades. After this, the mid-Piacenzian warmth enabled bi-directional fauna exchange between Africa and Eurasia, which continued during the Pleistocene.Transient periods of hyperaridity in northern Arabia during the late Miocene were out of phase with those in North Africa and may have promoted unidirectional dispersal of Eurasian mammals into Africa, according to analyses of a sedimentary sequence in western Iran.Alexander von Humboldt-Stiftung (Alexander von Humboldt Foundation) https://doi.org/10.13039/100005156https://doi.org/10.5281/zenodo.470478

    Neogene hyperaridity in Arabia drove the directions of mammalian dispersal between Africa and Eurasia

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    &lt;jats:title&gt;Abstract&lt;/jats:title&gt;&lt;jats:p&gt;The evolution of the present-day African savannah fauna has been substantially influenced by the dispersal of Eurasian ancestors into Africa. The ancestors evolved endemically, together with the autochthonous taxa, into extant Afrotropical clades during the last 5 million years. However, it is unclear why Eurasian ancestors moved into Africa. Here we use sedimentological observations and soluble salt geochemical analyses of samples from a sedimentary sequence in Western Iran to develop a 10-million-year long proxy record of Arabian climate. We identify transient periods of Arabian hyperaridity centred 8.75, 7.78, 7.50 and 6.25 million years ago, out-of-phase with Northern African aridity. We propose that this relationship promoted unidirectional mammalian dispersals into Africa. This was followed by a sustained hyperarid period between 5.6 and 3.3 million years ago which impeded dispersals and allowed African mammalian faunas to endemically diversify into present-day clades. After this, the mid-Piacenzian warmth enabled bi-directional fauna exchange between Africa and Eurasia, which continued during the Pleistocene.&lt;/jats:p&gt
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