Search results for "Feature"

showing 10 items of 4091 documents

The owl that never left! Taphonomy of Earlier Stone Age small mammal assemblages from Wonderwerk Cave (South Africa)

2022

Wonderwerk Cave, in South Africa, is an exceptional site that has yielded a large collection of small mammal fossils in a stratigraphic sequence reaching back ca. 2 million years. Taphonomic studies undertaken to date, show that Tytonidae (likely Tyto alba) was the dominant predator during the Earlier Stone Age. They produced masses of pellets that formed a dense carpet-like surface that covered the cave floor at intervals throughout the sequence. This paper compares the taphonomic signatures of five different Earlier Stone Age small mammal assemblages from Wonderwerk Cave, including assemblages not studied before, as well as a modern pellet assemblage collected from inside the cave. These …

010506 paleontologygeographygeography.geographical_feature_categoryTaphonomyTyto albabiologyRaptor pelletsPalaeoenvironmentTytoMicromammalsBarn owl010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesArchaeologyStone AgePredationCaveTytonidaePaleoecologyAssemblage (archaeology)Sequence stratigraphy0105 earth and related environmental sciencesEarth-Surface Processes
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Climatic ups and downs in a disturbed Jurassic world.

2011

4 pages; International audience; The tropical, warm, and equable climate of the Jurassic world is regularly challenged by geoscientists, especially since oxygen isotopes ( 18O) of fossil hardparts have been used to reconstruct the paleotemperature history of seawater. By applying the innovative “SiZer” (significant zero crossings of the derivatives) statistical approach to a newly compiled 18O database for the Jurassic, we demonstrate the occurrence of major and multiscale 18O changes mainly related to climate disturbances. For the first time, two long-term anomalies in 18O are identified during the Toarcian and the Late Jurassic, in conjunction with intensive volcanism in large igneous pro…

010506 paleontologygeographygeography.geographical_feature_category[SDE.MCG]Environmental Sciences/Global ChangesGeologyVolcanism010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenIgneous rockPaleontology[ SDE.MCG ] Environmental Sciences/Global ChangesVolcano13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIce caps[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyGeology0105 earth and related environmental sciences
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Paleoecological constraints on reef-coral morphologies in the Tortonian–early Messinian of the Lorca Basin, SE Spain

2004

Abstract Coral reefs represent one of the main carbonate factories that contributed to the control of the stratigraphic architecture of carbonate platforms, which had a widespread development during the late Miocene in the paleo-Mediterranean area. The late Miocene reef complexes of the Lorca Basin in southeastern Spain are composed of five mixed siliciclastic/carbonate units, middle Tortonian to early Messinian in age. The development of coral reefs probably ceased when the first evaporitic event occurred in the basin centre in the early Messinian. This study mainly focuses on the response of reef communities and the modifications of reef organisation to global and regional parameters. At …

010506 paleontologygeographygeography.geographical_feature_categorybiologyCarbonate platformCoralPoritesPaleontologyCoralline algaeCoral reefLate Miocene010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesPaleontologySiliciclastic14. Life underwaterReefEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Geological Setting and Paleoecology of the Upper Cretaceous Bench 19 Marine Vertebrate Bonebed at Bentiaba, Angola

2014

AbstractThe Bench 19 Bonebed at Bentiaba, Angola, is a unique concentration of marine vertebrates preserving six species of mosasaurs in sediments best correlated by magnetostratigraphy to chron C32n.1n between 71.4 and 71.64 Ma. The bonebed formed at a paleolatitude near 24°S, with an Atlantic width at that latitude approximating 2700 km, roughly half that of the current width. The locality lies on an uncharacteristically narrow continental shelf near transform faults that controlled the coastal outline of Africa in the formation of the South Atlantic Ocean. Biostratigraphic change through the Bentiaba section indicates that the accumulation occurred in an ecological time dimension within …

010506 paleontologygeographygeography.geographical_feature_categorybiologyContinental shelfFaunaGeology010502 geochemistry & geophysicsbiology.organism_classificationMosasaur01 natural sciencesCretaceous/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterPaleontologyMarine vertebratePrognathodonPaleoecology14. Life underwaterSDG 14 - Life Below WaterGeologyMagnetostratigraphy0105 earth and related environmental sciencesNetherlands Journal of Geosciences = Geologie en Mijnbouw
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Warming or cooling in the Pragian? Sedimentary record and petrophysical logs across the Lochkovian–Pragian boundary in the Spanish Central Pyrenees

2016

Abstract High-resolution petrophysical correlation methods were applied, for the first time, to mid-Paleozoic rocks of the Pyrenees. The methods included magnetic susceptibility measurements (MS), gamma-ray spectrometry (GRS), and alignment of MS logs using the dynamic time-warping (DTW) algorithm. Conodont biostratigraphy provided the basic framework necessary for work with the GRS and MS logs. Despite differences in the sediment patterns and accumulation/erosion rates, the logs from two selected sections in the Spanish Central Pyrenees show a striking symmetry that correlates well with the previously published logs from the Barrandian area in the Czech Republic. The high similarity betwee…

010506 paleontologygeographygeography.geographical_feature_categorybiologyPaleontologyClimate changeSedimentBiostratigraphy010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesPaleontologyPeriod (geology)Sedimentary rockIce sheetConodontEcology Evolution Behavior and SystematicsGeologySea level0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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ISOTOPIC TEMPERATURES FROM THE EARLY AND MID-PLIOCENE OF THE US MIDDLE ATLANTIC COASTAL PLAIN, AND THEIR IMPLICATIONS FOR THE CAUSE OF REGIONAL MARIN…

2017

Mean seasonal extreme temperatures on the seafloor calculated from the shell d 18 Oofthescallop Placopecten clintonius from the basal part of the early Pliocene Sunken Meadow Member (Yorktown Formation) in Virginia are very similar to those from the same horizon at the latitude of Cape Hatteras in North Carolina ( ~ 210 km to the south). The lowest and highest temperatures calculated from each shell (using d 18 O seawater ¼þ 0.7 % )givemean values for winter and summer of 8.4 6 1.1 8 C( 6 1 r ) and 18.2 6 0.6 8 CinVirginia,and8.6 6 0.4 8 Cand16.5 6 1.1 8 C in North Carolina (respective median temperatures: 13.3 8 C and 12.6 8 C). Patterns of ontogenetic variation in d 18 O, d 13 C and micro…

010506 paleontologygeographygeography.geographical_feature_categoryδ13CYorktown Formationδ18OCoastal plainPaleontologyOceanic climate010502 geochemistry & geophysics01 natural sciencesGulf StreamOceanographySclerochronologyPaleoclimatologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences
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A 4000-year long Late Holocene climate record from Hermes Cave (Peloponnese, Greece)

2020

The societal and cultural development during the Bronze Age and the subsequent Iron Age was enormous in Greece, however interrupted by two significant transformations around 4200 years b2k (Early Helladic II/III; b2k refers to years before 2000 CE) and 3200 years b2k (end of Late Helladic III). Artefacts and building remains provide some insights into the cultural evolution, but only little is known about environmental and climatic changes on a detailed temporal and spatial scale. Here we present a 4000-year long stalagmite record (GH17-05) from Hermes Cave, Greece, located on Mount Ziria in the close vicinity of the Late Bronze Age citadel of Mycenae and the Classical-Hellenistic polis of …

010506 paleontologygeographygeography.geographical_feature_categoryδ13Cδ18OSpeleothemStalagmite01 natural sciencesCaveBronze AgePaleoclimatologyPhysical geographyHoloceneGeology0105 earth and related environmental sciences
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New advances on the Aurignacian in the central Iberian Mediterranean basin

2021

Abstract This study aims to obtain a chronological and cultural framework of the Evolved Aurignacian in the central Iberian Mediterranean basin and find agreement between this framework and other sequences of the Iberian southeast. Over the last few years, there has been remarkable progress in the research of the Evolved Aurignacian sites in the Valencian area, making a review of the main characteristics of the technocomplex on a regional scale necessary. The recent fieldwork carried out in Cova de les Malladetes (Valencia) and in Cova de les Cendres (Alicante) have been key to understanding the lithic, osseous and ornament assemblages ascribed to the Evolved Aurignacian. Several Bayesian m…

010506 paleontologygeography.geographical_feature_category060102 archaeology06 humanities and the arts01 natural sciencesMediterranean BasinArchaeologyCultural frameworkValencianlanguage.human_languageGeographyHistory and Philosophy of SciencePeninsulaAnthropologylanguage0601 history and archaeologyAurignacian0105 earth and related environmental sciencesL'Anthropologie
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Different parts of the same plants. Charcoals and seeds from Cova de les Cendres (Alicante, Spain)

2018

Abstract The analysis of archaeobotanical macroremains from Cova de les Cendres (Teulada-Moraira, Alicante, Spain) allows a better understanding of the dynamic of the vegetation during the Upper Palaeolithic in the region. The anthracological sequence shows that Pinus type nigra/sylvestris dominates in the area during the Upper Palaeolithic, while more open formations of Juniperus and Fabaceae spread in Upper Solutrean and Early-Middle Magdalenian. The carpological analysis that has been carried out in the Middle Magdalenian level has brought to light different species of Juniperus (J. sabina, J. communis and J. oxycedrus). This information indicates that during the period, Cova de les Cend…

010506 paleontologygeography.geographical_feature_category060102 archaeologybiologySteppeJuniperus sabina06 humanities and the artsVegetationbiology.organism_classificationSolutrean01 natural sciencesArchaeologyGeographyvisual_artvisual_art.visual_art_mediumPeriod (geology)0601 history and archaeologyGlacial periodMagdalenianCharcoal0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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Landscape and fuel management in the context of prehistoric and historical occupations of Cova des Moro (Manacor, Mallorca, Spain)

2021

Abstract In this paper, the first results of charcoal analyses carried out at Cova des Moro (Manacor, Mallorca, Spain) are presented. This cave is an archaeological but also palaeontological site that provides information on endemic fauna (the extinct caprine Myotragus balearicus) before the arrival of humans and, later, the relationship between the first farmers and the landscape. Several human occupations in the cave have been documented, from the Chalcolithic (end of the 3rd millennium cal BC), the Bronze Age (2nd millennium cal BC) and, finally, the Almohad period (13th century AD), during which the cave was used for different purposes. The first results of charcoal analyses at Cova des…

010506 paleontologygeography.geographical_feature_categorybiologyContext (language use)Chalcolithic010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesArchaeologyMyotragusPrehistoryGeographyCaveAleppo PineBronze AgeJuniper0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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