Search results for "oceanography"

showing 10 items of 1567 documents

Five centuries of Central European temperature extremes reconstructed from tree-ring density and documentary evidence

2010

Future climate change will likely influence the frequency and intensity of weather extremes. As such events are by definition rare, long records are required to understand their characteristics, drivers, and consequences on ecology and society. Herein we provide a unique perspective on regional-scale temperature extremes over the past millennium, using three tree-ring maximum latewood density (MXD) chronologies from higher elevations in the European Alps. We verify the tree-ring-based extremes using documentary evidences from Switzerland, the Czech Republic, and Central Europe that allowed the identification of 44 summer extremes over the 1550-2003 period. These events include cold temperat…

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesCentral EuropeClimate changeContext (language use)DendroclimatologyEuropean Alp15. Life on landOceanography01 natural sciencesDocumentary evidenceMaximum latewood densityDocumentary evidenceSpatial coherenceTemperature extremeGeographyPalaeoclimatology13. Climate actionClimatologyPaleoclimatologyPeriod (geology)Dendrochronology0105 earth and related environmental sciences
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The ELSA-Flood-Stack: A reconstruction from the laminated sediments of Eifel maar structures during the last 60 000 years

2016

Abstract This study reconstructs the main flood phases in central Europe from event layers in sediment cores from Holocene Eifel maar lakes and Pleistocene dry maar structures. These reconstructions are combined with recent gauge time-series to cover the entire precipitation extremes of the last 60 000 years. In general, Eifel maar sediments are perfectly suited for the preservation of event layers since the deep water in the maar lakes is seasonal anoxic and therefore, bioturbation is low. However, the preservation of annual lamination is only preserved in Holzmaar and Ulmener Maar; the other cores are dated by 14C, magnetostratigraphy, tephra markers and ice core tuning. The cores were dr…

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesFlood mythOceanography01 natural sciencesMaarIce corePaleoclimatologyPhysical geographyYounger DryasStadialGlacial periodGeomorphologyGeologyHolocene0105 earth and related environmental sciencesGlobal and Planetary Change
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The ELSA - Stacks (Eifel-Laminated-Sediment-Archive): An introduction

2016

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesGeochemistrySedimentOceanography01 natural sciencesGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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The ELSA tephra stack: Volcanic activity in the Eifel during the last 500,000 years

2016

Abstract Tephra layers of individual volcanic eruptions are traced in several cores from Eifel maar lakes, drilled between 1998 and 2014 by the Eifel Laminated Sediment Archive (ELSA). All sediment cores are dated by 14C and tuned to the Greenland interstadial succession. Tephra layers were characterized by the petrographic composition of basement rock fragments, glass shards and characteristic volcanic minerals. 10 marker tephra, including the well-established Laacher See Tephra and Dumpelmaar Tephra can be identified in the cores spanning the last glacial cycle. Older cores down to the beginning of the Elsterian, show numerous tephra sourced from Strombolian and phreatomagmatic eruptions,…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEarth scienceGeochemistry010502 geochemistry & geophysicsOceanography01 natural sciencesLapilliStrombolian eruptionMaarVolcanoMagmaPhreatomagmatic eruptionTephraTephrochronologyGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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Recent advances in paleoflood hydrology: From new archives to data compilation and analysis

2018

8 pags, 4 figs

010506 paleontologyHistory010504 meteorology & atmospheric sciencesFlood frequency analysismedia_common.quotation_subjectFluvialManagement Monitoring Policy and LawOceanography01 natural sciencesNatural (archaeology)ScarcityHydrology (agriculture)ddc:550ChallengesWaste Management and Disposal0105 earth and related environmental sciencesWater Science and Technologymedia_commonHydrologyddc:333.7-333.9Paleoflood hydrologyFlood mythField historyAdvances13. Climate actionFlood hazardData compilationFlood hazardNatural archives
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Conjunctive use of spectral gamma-ray logs and clay mineralogy in defining late Jurassic-early Cretaceous palaeoclimate change (Dorset, U.K.).

2006

Abstract Detrital clay mineralogy is controlled by weathered source rock, climate, transport and deposition that in turn influence the spectral gamma-ray (SGR) response of resultant sediments. Whilst a palaeoclimate signal in clay mineralogy has been established in some ancient successions, the SGR response remains contentious, largely because the data sets have yet to be collected at the same or appropriate vertical scales to allow comparison. In addition, the influence of organic matter on SGR is not always considered. Here, we present clay mineralogical, total organic carbon (TOC) and SGR analyses from the late Jurassic and early Cretaceous of the Wessex Basin, a period of previously doc…

010506 paleontologyJurassic-Cretaceous boundary[SDE.MCG]Environmental Sciences/Global ChangesSpectral gamma raychemistry.chemical_elementStructural basin010502 geochemistry & geophysicsOceanographyPalaeoclimate[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontology[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgDorsetKaoliniteOrganic matter[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/MineralogyEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbonchemistry.chemical_classificationPaleontologyThoriumClay mineralogyCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesSource rockchemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPurbeck facies[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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High-resolution geochemical and biotic records of the Tethyan 'Bonarelli Level' (OAE2, latest Cenomanian) from the Calabianca-Guidaloca composite sec…

2004

Abstract High-resolution micropalaeontological and chemostratigraphic records for the upper Cenomanian portion of the Calabianca–Guidaloca composite section (NW Sicily) provide new insight into the palaeoclimatic and palaeoceanographic evolution of the Tethys Ocean. The Bonarelli Level equivalent was identified on the basis of lithology and well constrained by calcareous plankton biostratigraphy and radiolarian assemblages, as well as by the δ 13 C curve showing a marked positive excursion (up to 4.7‰). The Bonarelli Level equivalent deposition is characterized by highly eutrophic conditions as testified by radiolarian proliferation. Black shale samples from the Calabianca–Guidaloca composi…

010506 paleontologyLithologyBiostratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesMicrofossilsCretaceousForaminiferaPaleontologyPalaeoceanography14. Life underwaterSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyPaleontologyCretaceous Sicily Corg-rich deposits Bonarelli level equivalent Microfossils Geochemical proxies Palaeoceanography15. Life on landbiology.organism_classificationTethys OceanAnoxic watersCretaceous13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBonarelli level equivalentCenomanianGeology
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Early Pliocene continental vertebrate fauna at Puerto de la Cadena (SE Spain) and its bearing on the marine-continental correlation of the Late Neoge…

2017

In this paper, we synthesize sedimentological, magnetostratigraphic and paleontological data from the continental vertebrate site of Puerto de la Cadena (Murcia, SE Spain), in order to clarify its age. The study site is located on the northern edge of the Carrascoy mountain range, in the upper part of the Cigarrón Unit. The end-Messinian discontinuity has been detected at the base of this unit, which indicates it has an early Pliocene age. Abundant remains of small and large vertebrates, including rodents, lagomorphs, primates, carnivorans, perissodactyls, artiodactyls, proboscideans, testudines, squamats, and crocodiles, have been found in this area. Some of these elements are of African o…

010506 paleontologyMessinian salinity crisisFaunaEstratigrafíaLate MioceneBiostratigraphy010502 geochemistry & geophysicsOceanographyNeogene01 natural sciencesPaleontologybiology.animalSivatheriumEcology Evolution Behavior and SystematicsMagnetostratigraphy0105 earth and related environmental sciencesEarth-Surface ProcessesMammalsbiologyEcologyMagnetostratigraphyPaleontologyVertebrateReptilesBiostratigraphybiology.organism_classificationHipparionGeologyIberian Peninsula
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Bone diagenesis in arid environments; An intra-skeletal approach

2014

Bone trace element content and isotopic composition are closely related to human nutrition. The investigation of archaeological bone geochemistry can help us to better understand the relationship between past populations and their environment alongside cultural practices as inferred from dietary reconstruction. However, dietary in- formation may be altered post-mortem by diagenetic processes in soil. In this study, bone mineralogy (Ca/P, sec- ondary minerals, organic matter content and bone apatite crystallinity), histology, element content (Mg, Na, F, Sr, Ba, Mn, Fe, La, Ce and U) and stable isotope composition (δ13Candδ18O carbonate) were investigated at the intra- individual scale in ord…

010506 paleontologyMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesOceanography01 natural sciencesApatitechemistry.chemical_compound0601 history and archaeologyOrganic matterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeschemistry.chemical_classification060102 archaeologyEnamel paintStable isotope ratioBioerosionTrace elementPaleontology06 humanities and the artsDiagenesischemistryvisual_artvisual_art.visual_art_mediumCarbonateGeology
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Erratum to “Palaeoecological context for the extinction of the Neanderthals: A small mammal study of Stratigraphic Unit V of the El Salt site, Alcoi,…

2021

El Salt is an important reference site for understanding the extinction of Neanderthal populations in the eastern Iberian Peninsula during MIS 3. In this paper, we describe the small mammal assemblage from Stratigraphic Unit V, the youngest unit with evidence of human presence, based on nearly 1300 specimens. A total of seven rodents (Microtus arvalis, Microtus duodecimcostatus, Microtus cabrerae, Sciurus vulgaris, Arvicola sapidus, Eliomys quercinus and Apodemus sylvaticus), three insectivores (Talpa occidentalis, Crocidura sp., Sorex sp.) and one lagomorph (Oryctolagus cf. cuniculus) were identified. Palaeocological analyses point to drier conditions in this part of the stratigraphic sequ…

010506 paleontologyNeanderthalZoologySorex010502 geochemistry & geophysicsOceanography01 natural sciencesMicrotus cabrerae//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]El SaltCrocidurabiology.animalSmall mammalsEliomysMicrotusEcology Evolution Behavior and SystematicsNeanderthals0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyMicrotus duodecimcostatusPaleontologyExtinctionbiology.organism_classificationPleistocenePalaeoclimatologyArvicolaGeologyIberian PeninsulaPalaeogeography, Palaeoclimatology, Palaeoecology
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