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  • 1
    Publication Date: 2014-12-04
    Description: The manufacture of geometric engravings is generally interpreted as indicative of modern cognition and behaviour. Key questions in the debate on the origin of such behaviour are whether this innovation is restricted to Homo sapiens, and whether it has a uniquely African origin. Here we report on a fossil freshwater shell assemblage from the Hauptknochenschicht ('main bone layer') of Trinil (Java, Indonesia), the type locality of Homo erectus discovered by Eugene Dubois in 1891 (refs 2 and 3). In the Dubois collection (in the Naturalis museum, Leiden, The Netherlands) we found evidence for freshwater shellfish consumption by hominins, one unambiguous shell tool, and a shell with a geometric engraving. We dated sediment contained in the shells with (40)Ar/(39)Ar and luminescence dating methods, obtaining a maximum age of 0.54 +/- 0.10 million years and a minimum age of 0.43 +/- 0.05 million years. This implies that the Trinil Hauptknochenschicht is younger than previously estimated. Together, our data indicate that the engraving was made by Homo erectus, and that it is considerably older than the oldest geometric engravings described so far. Although it is at present not possible to assess the function or meaning of the engraved shell, this discovery suggests that engraving abstract patterns was in the realm of Asian Homo erectus cognition and neuromotor control.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Joordens, Josephine C A -- d'Errico, Francesco -- Wesselingh, Frank P -- Munro, Stephen -- de Vos, John -- Wallinga, Jakob -- Ankjaergaard, Christina -- Reimann, Tony -- Wijbrans, Jan R -- Kuiper, Klaudia F -- Mucher, Herman J -- Coqueugniot, Helene -- Prie, Vincent -- Joosten, Ineke -- van Os, Bertil -- Schulp, Anne S -- Panuel, Michel -- van der Haas, Victoria -- Lustenhouwer, Wim -- Reijmer, John J G -- Roebroeks, Wil -- England -- Nature. 2015 Feb 12;518(7538):228-31. doi: 10.1038/nature13962. Epub 2014 Dec 3.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Faculty of Archaeology, Leiden University, PO Box 9515, 2300RA, Leiden, The Netherlands [2] Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081HV, Amsterdam, The Netherlands. ; 1] Universite de Bordeaux, CNRS UMR 5199, Allee Geoffroy Saint-Hilaire, 33615 Pessac, France [2] Institute of Archaeology, History, Cultural Studies and Religion, University of Bergen, Oysteinsgate 3PO Box 7805, Bergen, Norway. ; Naturalis Biodiversity Center, Darwinweg 2, PO Box 9517, 2300RA, Leiden, The Netherlands. ; 1] School of Archaeology and Anthropology, Australian National University, Australian Capital Territory, 0200 Canberra, Australia [2] National Museum of Australia, Australian Capital Territory 2601, Canberra, Australia. ; 1] Wageningen University, Soil Geography and Landscape Group &Netherlands Centre for Luminescence Dating, PO Box 47, 6700AA, Wageningen, The Netherlands [2] Delft University of Technology, Faculty of Applied Sciences, Mekelweg 15, 2629JB, Delft, The Netherlands. ; Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081HV, Amsterdam, The Netherlands. ; 1] Faculty of Archaeology, Leiden University, PO Box 9515, 2300RA, Leiden, The Netherlands [2] Prinses Beatrixsingel 21, 6301VK, Valkenburg, The Netherlands. ; Universite de Bordeaux, CNRS UMR 5199, Allee Geoffroy Saint-Hilaire, 33615 Pessac, France. ; 1] Museum National d'Histoire Naturelle, UMR 7205, Institut de Systematique, Evolution, Biodiversite, CP51, 55 Rue Buffon, 75005 Paris, France [2] Biotope Recherche et Developpement, 22 Boulevard Marechal Foch, 34140 Meze, France. ; Cultural Heritage Agency of the Netherlands, PO Box 1600, 3800BP, Amersfoort, The Netherlands. ; 1] Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081HV, Amsterdam, The Netherlands [2] Naturalis Biodiversity Center, Darwinweg 2, PO Box 9517, 2300RA, Leiden, The Netherlands [3] Natuurhistorisch Museum Maastricht, De Bosquetplein 7, 6211KJ, Maastricht, The Netherlands. ; 1] Faculte de Medecine, Universite d'Aix-Marseille, EFS, CNRS UMR 7268, Boulevard Pierre Dramard, 13344 Marseille, France [2] Department of Medical Imaging Hopital Nord, Assistance Publique - Hopitaux de Marseille, Chemin de Bourrellys, 13915 Marseille, France. ; Faculty of Archaeology, Leiden University, PO Box 9515, 2300RA, Leiden, The Netherlands.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25470048" target="_blank"〉PubMed〈/a〉
    Keywords: *Animal Shells ; Animals ; Engraving and Engravings/*history ; Fossils ; History, Ancient ; *Hominidae ; Indonesia ; Mollusca ; *Tool Use Behavior
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2008-08-02
    Description: Hotspots of high species diversity are a prominent feature of modern global biodiversity patterns. Fossil and molecular evidence is starting to reveal the history of these hotspots. There have been at least three marine biodiversity hotspots during the past 50 million years. They have moved across almost half the globe, with their timing and locations coinciding with major tectonic events. The birth and death of successive hotspots highlights the link between environmental change and biodiversity patterns. The antiquity of the taxa in the modern Indo-Australian Archipelago hotspot emphasizes the role of pre-Pleistocene events in shaping modern diversity patterns.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Renema, W -- Bellwood, D R -- Braga, J C -- Bromfield, K -- Hall, R -- Johnson, K G -- Lunt, P -- Meyer, C P -- McMonagle, L B -- Morley, R J -- O'Dea, A -- Todd, J A -- Wesselingh, F P -- Wilson, M E J -- Pandolfi, J M -- New York, N.Y. -- Science. 2008 Aug 1;321(5889):654-7. doi: 10.1126/science.1155674.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Nationaal Natuurhistorisch Museum, Naturalis, 2300 RA, Leiden, Netherlands. Renema@naturalis.nl〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18669854" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Anthozoa/classification ; *Biodiversity ; Climate ; Ecosystem ; Fishes/classification ; *Fossils ; Geological Phenomena ; Geology ; *Marine Biology ; Mollusca/classification ; Phylogeny ; Rhizophoraceae/classification ; *Seawater ; Time
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2010-11-13
    Description: The Amazonian rainforest is arguably the most species-rich terrestrial ecosystem in the world, yet the timing of the origin and evolutionary causes of this diversity are a matter of debate. We review the geologic and phylogenetic evidence from Amazonia and compare it with uplift records from the Andes. This uplift and its effect on regional climate fundamentally changed the Amazonian landscape by reconfiguring drainage patterns and creating a vast influx of sediments into the basin. On this "Andean" substrate, a region-wide edaphic mosaic developed that became extremely rich in species, particularly in Western Amazonia. We show that Andean uplift was crucial for the evolution of Amazonian landscapes and ecosystems, and that current biodiversity patterns are rooted deep in the pre-Quaternary.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hoorn, C -- Wesselingh, F P -- ter Steege, H -- Bermudez, M A -- Mora, A -- Sevink, J -- Sanmartin, I -- Sanchez-Meseguer, A -- Anderson, C L -- Figueiredo, J P -- Jaramillo, C -- Riff, D -- Negri, F R -- Hooghiemstra, H -- Lundberg, J -- Stadler, T -- Sarkinen, T -- Antonelli, A -- New York, N.Y. -- Science. 2010 Nov 12;330(6006):927-31. doi: 10.1126/science.1194585.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Paleoecology and Landscape Ecology, Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, Science Park 904, 1098 XH Amsterdam, Netherlands. carina.hoorn@milne.cc〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21071659" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Biodiversity ; *Climate Change ; Ecosystem ; Fossils ; Geography ; *Geological Phenomena ; Phylogeny ; Rivers ; South America ; Time ; Trees ; Wetlands
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2017-05-04
    Description: There is a considerable controversy about whether western Amazonia was ever covered by marine waters during the Miocene [23 to 5 Ma (million years ago)]. We investigated the possible occurrence of Miocene marine incursions in the Llanos and Amazonas/Solimões basins, using sedimentological and palynological data from two sediment cores taken in eastern Colombia and northwestern Brazil together with seismic information. We observed two distinct marine intervals in the Llanos Basin, an early Miocene that lasted ~0.9 My (million years) (18.1 to 17.2 Ma) and a middle Miocene that lasted ~3.7 My (16.1 to 12.4 Ma). These two marine intervals are also seen in Amazonas/Solimões Basin (northwestern Amazonia) but were much shorter in duration, ~0.2 My (18.0 to 17.8 Ma) and ~0.4 My (14.1 to 13.7 Ma), respectively. Our results indicate that shallow marine waters covered the region at least twice during the Miocene, but the events were short-lived, rather than a continuous full-marine occupancy of Amazonian landscape over millions of years.
    Electronic ISSN: 2375-2548
    Topics: Natural Sciences in General
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  • 5
    Publication Date: 2015-02-27
    Description: Two late Miocene Tridacna (giant clam) shells from East Kalimantan (Indonesia) were investigated in order to evaluate their potential as subannually resolved paleoenvironmental archives. Via a combination of X-ray diffraction (XRD), laser ablation–inductively coupled plasma–mass spectrometry (LA-ICPMS) trace element analysis, scanning electron microscopy (SEM) and cathodoluminescence (CL) imaging, pristine versus diagenetically altered domains within the shells were identified. LA-ICPMS transects targeting altered aragonite and calcite zones reveal distinct compositional differences in elemental ratios (B/Ca, Mg/Ca, Sr/Ca/ Ba/Ca, Mn/Ca, Al/Ca, La/Ca, Ce/Ca) relative to primary shell aragonite. Pristine shell domains are characterized by an intact banding pattern of alternating dark and light growth bands, with which spatially resolved LA-ICPMS element/Ca and micromilled 18 O records were aligned. Light 18 O values correspond to dark growth bands, indicating growth during warm seasons. The Mg/Ca and/or Sr/Ca ratios covary with oscillating stable oxygen isotope profiles. Progressive increase in Mg/Ca with age demonstrates that besides temperature, growth kinetics exert control over Mg incorporation. If interpreted as temperature controlled only, 18 O from both shells represents average seasonal sea-surface temperature (SST) variability of 2.7 ± 2.1 and 4.6 ± 1.7 °C, respectively. Using published temperature equations and assuming 18 O sw = –0.88, corresponding mean annual paleo–sea-surface temperatures of 27.8 ± 0.2 and 28.5 ± 0.2 °C are estimated. Although the fossil Tridacna shells were noticeably affected by alteration on their external surfaces, their internal aragonitic structure is, to a large extent, well preserved. These corresponding paleoproxy records provide detailed insight into tropical SST variability of the Indo-Pacific region during the late Miocene.
    Print ISSN: 0883-1351
    Electronic ISSN: 0883-1351
    Topics: Geosciences
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  • 6
    Publication Date: 2015-02-27
    Description: This study is a preliminary assessment of an extremely diverse Tortonian (late Miocene) mollusk assemblage from a coral carpet environment preserved at Bontang (East Kalimantan, Indonesia). Even though coral-associated aragonitic faunas are rarely well preserved, the composition of the assemblage described here can be used to address the following questions: (1) How do the mollusk assemblages in coral habitats differ from other habitats, and (2) What is the effect of sampling on estimates of taxon richness? The mollusk assemblage is dominated by predatory snails and includes typical modern coral-associated taxa such as the gastropod Coralliophila and the bivalve Tridacna . Our investigation implies that adequate documentation of Cenozoic mollusk diversity in the Indo-Pacific is even more challenging than previously expected as very large samples are required to capture species richness. Further assessments of fossil faunas from coral-dominated habitats will be required to provide insight to development of Indo-Pacific biodiversity through time.
    Print ISSN: 0883-1351
    Electronic ISSN: 0883-1351
    Topics: Geosciences
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  • 7
    Publication Date: 2015-02-27
    Description: Seagrass meadows are important shallow-water ecosystems that provide habitat for numerous associated organisms and play a crucial role in nutrient cycling, but their detection in the fossil record is problematic. Indirect indicators are often needed to discriminate seagrass beds from other shallow marine paleohabitats. Here, the stable isotope signatures of mollusk shells are examined to determine if they might provide such an indicator in addition to the faunal composition of mollusk assemblages. Aragonitic shells of 167 gastropods and bivalves from Burdigalian and Tortonian deposits in Java and East Kalimantan (Indonesia) are analyzed for their 18 O and 13 C ratios. The faunas represent fully marine to brackish water environments and include seagrass meadows (with dispersed corals), mixed seagrass-coral, and coral-dominated habitats (with dispersed seagrass). We assess processes and settings that shape inorganic isotope signals in the Miocene ambient waters and fractionation processes occurring at the time of shell deposition. Depleted 18 O and 13 C ratios are shown in brackish water samples. Furthermore, chemosymbiotic species show depleted 13 C ratios. A significant difference is found between the carbon isotopic signatures of coral- and seagrass-dominated environments within a stratigraphic interval. Seagrass communities consistently yield comparatively enriched 13 C ratios. Hence, stable isotope ratios may provide additional evidence for distinguishing paleoenvironments and are helpful in identifying ecological processes and settings within these environments.
    Print ISSN: 0883-1351
    Electronic ISSN: 0883-1351
    Topics: Geosciences
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  • 8
    Publication Date: 2011-01-27
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 9
    Publication Date: 2015-02-23
    Print ISSN: 0883-1351
    Electronic ISSN: 0883-1351
    Topics: Geosciences
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  • 10
    Publication Date: 2015-02-23
    Print ISSN: 0883-1351
    Electronic ISSN: 0883-1351
    Topics: Geosciences
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