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  • 1
    Publication Date: 2015-01-12
    Description: SST trends measured in the Somalia region during the southwest monsoon season over the period 1982-2013 have shown the existence of a warming-cooling dipole. The positive spot, with a warming trend on the order of 0.37ºC dec -1 , is centered around 5.1 ºN – 50.3º E and the negative one, with a trend on the order of -0.43ºC dec -1 , around 11.1 ºN – 52.2º E. The migration of the Great Whirl (GW) over the last three decades at a speed of -0.3 deg dec -1 in longitude and -0.6 deg dec -1 in latitude was considered as the possible origin of the SST dipole. The displacement of the GW produces changes in the geostrophic currents which, in turn, generate changes in the amount of advected water from and to coast. This article is protected by copyright. All rights reserved.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2015-11-26
    Description: Ancient DNA makes it possible to observe natural selection directly by analysing samples from populations before, during and after adaptation events. Here we report a genome-wide scan for selection using ancient DNA, capitalizing on the largest ancient DNA data set yet assembled: 230 West Eurasians who lived between 6500 and 300 bc, including 163 with newly reported data. The new samples include, to our knowledge, the first genome-wide ancient DNA from Anatolian Neolithic farmers, whose genetic material we obtained by extracting from petrous bones, and who we show were members of the population that was the source of Europe's first farmers. We also report a transect of the steppe region in Samara between 5600 and 300 bc, which allows us to identify admixture into the steppe from at least two external sources. We detect selection at loci associated with diet, pigmentation and immunity, and two independent episodes of selection on height.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Mathieson, Iain -- Lazaridis, Iosif -- Rohland, Nadin -- Mallick, Swapan -- Patterson, Nick -- Roodenberg, Songul Alpaslan -- Harney, Eadaoin -- Stewardson, Kristin -- Fernandes, Daniel -- Novak, Mario -- Sirak, Kendra -- Gamba, Cristina -- Jones, Eppie R -- Llamas, Bastien -- Dryomov, Stanislav -- Pickrell, Joseph -- Arsuaga, Juan Luis -- de Castro, Jose Maria Bermudez -- Carbonell, Eudald -- Gerritsen, Fokke -- Khokhlov, Aleksandr -- Kuznetsov, Pavel -- Lozano, Marina -- Meller, Harald -- Mochalov, Oleg -- Moiseyev, Vyacheslav -- Guerra, Manuel A Rojo -- Roodenberg, Jacob -- Verges, Josep Maria -- Krause, Johannes -- Cooper, Alan -- Alt, Kurt W -- Brown, Dorcas -- Anthony, David -- Lalueza-Fox, Carles -- Haak, Wolfgang -- Pinhasi, Ron -- Reich, David -- GM100233/GM/NIGMS NIH HHS/ -- Howard Hughes Medical Institute/ -- England -- Nature. 2015 Dec 24;528(7583):499-503. doi: 10.1038/nature16152. Epub 2015 Nov 23.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Genetics, Harvard Medical School, Boston, Massachusetts 02115, USA. ; Broad Institute of MIT and Harvard, Cambridge, Massachusetts 02142, USA. ; Howard Hughes Medical Institute, Harvard Medical School, Boston, Massachusetts 02115, USA. ; Independent researcher, Santpoort-Noord, The Netherlands. ; School of Archaeology and Earth Institute, Belfield, University College Dublin, Dublin 4, Ireland. ; Institute for Anthropological Research, Zagreb 10000, Croatia. ; Department of Anthropology, Emory University, Atlanta, Georgia 30322, USA. ; Smurfit Institute of Genetics, Trinity College Dublin, Dublin 2, Ireland. ; Australian Centre for Ancient DNA, School of Biological Sciences &Environment Institute, University of Adelaide, Adelaide, South Australia 5005, Australia. ; Laboratory of Human Molecular Genetics, Institute of Molecular and Cellular Biology, Siberian Branch of the Russian Academy of Sciences, Novosibirsk 630090, Russia. ; Department of Paleolithic Archaeology, Institute of Archaeology and Ethnography, Siberian Branch of the Russian Academy of Sciences, Novosibirsk 630090, Russia. ; Centro Mixto UCM-ISCIII de Evolucion y Comportamiento Humanos, 28040 Madrid, Spain. ; Departamento de Paleontologia, Facultad Ciencias Geologicas, Universidad Complutense de Madrid, 28040 Madrid, Spain. ; Centro Nacional de Investigacion sobre Evolucion Humana (CENIEH), 09002 Burgos, Spain. ; IPHES. Institut Catala de Paleoecologia Humana i Evolucio Social, Campus Sescelades-URV, 43007 Tarragona, Spain. ; Area de Prehistoria, Universitat Rovira i Virgili (URV), 43002 Tarragona, Spain. ; Netherlands Institute in Turkey, Istiklal Caddesi, Nur-i Ziya Sokak 5, Beyog lu 34433, Istanbul, Turkey. ; Volga State Academy of Social Sciences and Humanities, Samara 443099, Russia. ; State Office for Heritage Management and Archaeology Saxony-Anhalt and State Museum of Prehistory, D-06114 Halle, Germany. ; Peter the Great Museum of Anthropology and Ethnography (Kunstkamera) RAS, St Petersburg 199034, Russia. ; Department of Prehistory and Archaeology, University of Valladolid, 47002 Valladolid, Spain. ; The Netherlands Institute for the Near East, Leiden RA-2300, the Netherlands. ; Max Planck Institute for the Science of Human History, D-07745 Jena, Germany. ; Institute for Archaeological Sciences, University of Tubingen, D-72070 Tubingen, Germany. ; Danube Private University, A-3500 Krems, Austria. ; Institute for Prehistory and Archaeological Science, University of Basel, CH-4003 Basel, Switzerland. ; Anthropology Department, Hartwick College, Oneonta, New York 13820, USA. ; Institute of Evolutionary Biology (CSIC-Universitat Pompeu Fabra), 08003 Barcelona, Spain.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26595274" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/history ; Asia/ethnology ; Body Height/genetics ; Bone and Bones ; DNA/genetics/isolation & purification ; Diet/history ; Europe/ethnology ; Genetics, Population ; Genome, Human/*genetics ; Haplotypes/genetics ; History, Ancient ; Humans ; Immunity/genetics ; Male ; Multifactorial Inheritance/genetics ; Pigmentation/genetics ; Selection, Genetic/*genetics ; Sequence Analysis, DNA
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2013-12-07
    Description: Excavations of a complex of caves in the Sierra de Atapuerca in northern Spain have unearthed hominin fossils that range in age from the early Pleistocene to the Holocene. One of these sites, the 'Sima de los Huesos' ('pit of bones'), has yielded the world's largest assemblage of Middle Pleistocene hominin fossils, consisting of at least 28 individuals dated to over 300,000 years ago. The skeletal remains share a number of morphological features with fossils classified as Homo heidelbergensis and also display distinct Neanderthal-derived traits. Here we determine an almost complete mitochondrial genome sequence of a hominin from Sima de los Huesos and show that it is closely related to the lineage leading to mitochondrial genomes of Denisovans, an eastern Eurasian sister group to Neanderthals. Our results pave the way for DNA research on hominins from the Middle Pleistocene.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Meyer, Matthias -- Fu, Qiaomei -- Aximu-Petri, Ayinuer -- Glocke, Isabelle -- Nickel, Birgit -- Arsuaga, Juan-Luis -- Martinez, Ignacio -- Gracia, Ana -- de Castro, Jose Maria Bermudez -- Carbonell, Eudald -- Paabo, Svante -- England -- Nature. 2014 Jan 16;505(7483):403-6. doi: 10.1038/nature12788. Epub 2013 Dec 4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Evolutionary Genetics, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, 04103 Leipzig, Germany. ; 1] Department of Evolutionary Genetics, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, 04103 Leipzig, Germany [2] Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China. ; 1] Centro de Investigacion Sobre la Evolucion y Comportamiento Humanos, Universidad Complutense de Madrid-Instituto de Salud Carlos III, 28029 Madrid, Spain [2] Departamento de Paleontologia, Facultad de Ciencias Geologicas, Universidad Complutense de Madrid, 28040 Madrid, Spain. ; 1] Centro de Investigacion Sobre la Evolucion y Comportamiento Humanos, Universidad Complutense de Madrid-Instituto de Salud Carlos III, 28029 Madrid, Spain [2] Area de Paleontologia, Depto. de Geografia y Geologia, Universidad de Alcala, Alcala de Henares, 28871 Madrid, Spain. ; Centro Nacional de Investigacion sobre la Evolucion Humana, Paseo Sierra de Atapuerca, 09002 Burgos, Spain. ; 1] Institut Catala de Paleoecologia Humana i Evolucio Social, C/Marcel.li Domingo s/n (Edifici W3), Campus Sescelades, 43007 Tarragona, Spain [2] Area de Prehistoria, Dept. d'Historia i Historia de l'Art, Univ. Rovira i Virgili, Fac. de Lletres, Av. Catalunya, 35, 43002 Tarragona, Spain.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24305051" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Bayes Theorem ; Consensus Sequence/genetics ; Cytosine/metabolism ; DNA, Mitochondrial/genetics ; Deamination ; Femur/anatomy & histology/metabolism ; *Fossils ; Genome, Mitochondrial/*genetics ; Hominidae/anatomy & histology/*classification/*genetics ; Molecular Sequence Data ; Neanderthals/genetics ; *Phylogeny ; Spain
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2015-10-16
    Description: The hominin record from southern Asia for the early Late Pleistocene epoch is scarce. Well-dated and well-preserved fossils older than approximately 45,000 years that can be unequivocally attributed to Homo sapiens are lacking. Here we present evidence from the newly excavated Fuyan Cave in Daoxian (southern China). This site has provided 47 human teeth dated to more than 80,000 years old, and with an inferred maximum age of 120,000 years. The morphological and metric assessment of this sample supports its unequivocal assignment to H. sapiens. The Daoxian sample is more derived than any other anatomically modern humans, resembling middle-to-late Late Pleistocene specimens and even contemporary humans. Our study shows that fully modern morphologies were present in southern China 30,000-70,000 years earlier than in the Levant and Europe. Our data fill a chronological and geographical gap that is relevant for understanding when H. sapiens first appeared in southern Asia. The Daoxian teeth also support the hypothesis that during the same period, southern China was inhabited by more derived populations than central and northern China. This evidence is important for the study of dispersal routes of modern humans. Finally, our results are relevant to exploring the reasons for the relatively late entry of H. sapiens into Europe. Some studies have investigated how the competition with H. sapiens may have caused Neanderthals' extinction (see ref. 8 and references therein). Notably, although fully modern humans were already present in southern China at least as early as approximately 80,000 years ago, there is no evidence that they entered Europe before approximately 45,000 years ago. This could indicate that H. neanderthalensis was indeed an additional ecological barrier for modern humans, who could only enter Europe when the demise of Neanderthals had already started.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Liu, Wu -- Martinon-Torres, Maria -- Cai, Yan-jun -- Xing, Song -- Tong, Hao-wen -- Pei, Shu-wen -- Sier, Mark Jan -- Wu, Xiao-hong -- Edwards, R Lawrence -- Cheng, Hai -- Li, Yi-yuan -- Yang, Xiong-xin -- de Castro, Jose Maria Bermudez -- Wu, Xiu-jie -- England -- Nature. 2015 Oct 29;526(7575):696-9. doi: 10.1038/nature15696. Epub 2015 Oct 14.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China. ; UCL Anthropology, 14 Taviton Street, London WC1H 0BW, UK. ; Departamento de Ciencias Historicas y Geografia. University of Burgos. Hospital del Rey, s/n. 09001 Burgos, Spain. ; Centro Nacional de Investigacion sobre la Evolucion Humana (CENIEH), Paseo Sierra de Atapuerca 3, 09002 Burgos, Spain. ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710075, China. ; Paleomagnetic Laboratory 'Fort Hoofddijk', Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Budapestlaan 17, 3584 CD Utrecht, The Netherlands. ; Faculty of Archaeology, Leiden University, PO Box 9515, 2300 RA Leiden, The Netherlands. ; School of Archaeology and Museology, Peking University, Beijing 100871, China. ; Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA. ; Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China. ; Institute of Cultural Relics and Archaeology, Hunan Province, Changsha 410008, China. ; Cultural Relics Administration of Daoxian County, Daoxian 425300, China.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26466566" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
    ISSN: 0006-3592
    Keywords: nitrification ; immobilized cells ; activation energy ; diffusion limitation ; temperature ; Chemistry ; Biochemistry and Biotechnology
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Activation energies of suspended and immobilized nitrifying bacteria were determined and compared to determine if diffusion limitation results in decreased sensitivity for temperature. The activation energy for the respiration activity of suspended Nitrosomonas europaea and Nitrobacter agilis was found to be 86.4 and 58.4 kJ mol-1, respectively. The activation energy for oxygen diffusion in the support material, κ-carrageenan, determined from the effect of temperature on the effective diffusion coefficient (D), was 17.2 kJ mol-1. Consequently, the apparent actvation energy of diffusion limited cells should be lower. It was indeed shown that due to the effect of diffusion limitation and to temperature effects on the Monod constant Ks, the immobilized-cell activity was less sensitive to temperature. The apparent activation energy for immobilized Ns. europaea was between 28.6 and 94.2 kJ mol-1 and for immobilized Nb. agilis between 1.4 and 72.9 kJ mol-1, depending on the oxygen concentration and temperature. © 1995 John Wiley & Sons, Inc.
    Additional Material: 8 Ill.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1824-310X
    Keywords: Pleistocene ; middle—cave infilling ; fossil record ; fossil hominids ; occupation floor ; acheulian
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The Atapuerca railway Trench and Ibeas sites near Burgos, Spain, are cave fillings that include a series of deposits ranging from below the Matuyama/Bruhnes reversal up to the end of Middle Pleistocene. The lowest fossil-bearing bed in the Trench contains an assemblage of large and small Mammals includingMimomys savini, Pitymys gregaloides, Pliomys episcopalis, Crocuta crocuta, Dama sp. and Megacerini; the uppermost assemblage includesCanis lupus, Lynx spelaea, Panthera (Leo) fossilis, Felis sylvestris, Equus caballus steinbeimensis, E.c. germanicus, Pitymys subterraneus, Microtus arvalis agrestis, Pliomys lenki, and alsoPanthera toscana, Dicerorbinus hemitoechus, Bison schoetensacki, which are equally present in the lowest level. The biostratigraphic correlation and dates of the sites are briefly discussed, as are the paleoclimatic interpretation of the Trench sequences. Stone artifacts are found in several layers; the earliest occurrences correspond to the upper beds containingMimomys savini. A set of preserved human occupation floors has been excavated in the top fossil-bearing beds. The stone-tool assemblages of the upper levels are of upper-medial Acheulean to Charentian tradition. The rich bone breccia SH, in the Cueva Mayor-Cueva del Silo, Ibeas de Juarros, is a derived deposit, due to a mud flow that dispersed and carried the skeletons of many carnivores and humans. The taxa represented are:Ursus deningeri (largely dominant),Panthera (Leo) fossilis, Vulpes vulpes, Homo sapiens var. Several traits of both mandibular and cranial remains are summarized. Preliminary attempts at dating suggest that the Ibeas fossil man is older than the Last Interglacial, or oxygen-isotope stage 5.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Human evolution 11 (1996), S. 205-215 
    ISSN: 1824-310X
    Keywords: Hominids ; teeth ; premolar-size sequence ; regression analysis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The size relationship between the crown area of the lower canines (Cs), third (P3s) and fourth premolars (P4s), and first molars (M1s) in hominids is examined by means of the regression analysis. The lower P3 seem to be under the influence of those factors that control both the size of the anterior and posterior teeth, and the P4:P3 size ratio is related to the relative size of the anterior and posterior dentitions. So, the P4〉P3 sequence is associated with the megadontia and hipermegadontia of the posterior teeth, whereas the expansion of the anterior teeth produces the P3〉P4 sequence. We consider the P4:P3 size ratio as an excellent indicator of the taxonomic and philogenetic status of fossil hominids.
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