Search results for "Interglacial"

showing 10 items of 77 documents

A detailed analysis of the spatial distribution of Schöningen 13II-4 'Spear Horizon' faunal remains

2021

The Middle Pleistocene Schöningen 13II-4 'Spear Horizon' (Germany) is a key site for the study of human evolution, most notably for the discovery of Paleolithic wooden weaponry and evidence for developed hunting strategies. On the other hand, the 'Spear Horizon' offers an excellent opportunity to approach hominin spatial behavior, thanks to the richness of the archeological assemblage, its exceptional preservation, and the vast expanse of the excavated surface. Analyzing how space was used is essential for understanding hominin behavior at this unique open-air site and, from a wider perspective, for approaching how humans adapted to interglacial environments. In this article, we present an …

Middle PleistocenePleistoceneAdaptation BiologicalContext (language use)Spatial distributionBirdsPaleontologyGermanyZooarcheologyAssemblage (archaeology)AnimalsEcology Evolution Behavior and SystematicsIntrasite spatial archeologyMammalsSpatial AnalysisHorizon (archaeology)Tool Use BehaviorFossilsFishesHominidaeBiodiversityHuman spatial behaviorGeographyHuman evolutionAnthropologyInterglacialGeographic Information SystemsWeaponsFaunal assemblage
researchProduct

Mutual Climatic Range Methods for Quaternary Ostracods

2012

Abstract The development of Mutual Climatic Range (MCR) methods for ostracods has included the estimation of marine bottom-water palaeotemperatures, but it has focused mainly on the use of non-marine ostracods to infer past air temperatures. The Delorme analogue MCR method, using only those components of a fossil assemblage that co-exist today, has yielded mean annual air temperature and annual precipitation estimates for North American Quaternary sites. The Mutual Ostracod Temperature Range (MOTR) non-analogue MCR method utilises all species in a fossil assemblage; calibrations based on a European database have been applied to the estimation of mean July and January air temperatures for En…

OceanographybiologyPleistoceneRange (biology)OstracodInterglacialTable (landform)Glacial periodPhysical geographybiology.organism_classificationQuaternaryHoloceneGeology
researchProduct

Millennial-scale paleoenvironmental changes in the central Mediterranean during the Last Interglacial: comparison with European and Mediterranean rec…

2008

Paleoceanography last interglacial Sicily ChannelPaleoceanography MIS 5 Mediterranean
researchProduct

The palaeoecoloical potential of pollen records in caves: the case of Mediterranean Spain

1999

Abstract Important palynological sequences are reviewed from caves with archaeological interest in Mediterranean Spain. Upper Pleistocene sites include Abric Romani and Abric de l’Arbreda in NE Spain, and in SE Spain Cueva de la Carihuela, Cova Beneito, Cueva de Perneras, Cueva del Algarrobo and the Holocene Cova de l’Or and Cova de les Cendres. Carihuela has the longest sequence, starting in the last interglacial and covering most of the last glaciation. A pre-Wurm phase was followed by two glacial maxima separated by an interpleniglacial phase, and in the Lateglacial the Younger Dryas seems present. Whereas at Carihuela harsh pleniglacial conditions caused Mediterranean associations to di…

PalynologyArcheologyGlobal and Planetary Changegeography.geographical_feature_categoryPleistoceneGeologyContext (language use)ArchaeologyGeographyCaveInterglacialGlacial periodYounger DryasEcology Evolution Behavior and SystematicsHoloceneQuaternary Science Reviews
researchProduct

New human remains of Archaic Homo sapiens and Lower Palaeolithic industries from Visogliano (Duino Aurisina, Trieste, Italy).

2000

New human remains have been found during recent excavations conducted in the lower section of Visogliano dolina (Trieste, Italy). They are represented by teeth and a fragment of particularly robust mandible that for their morphological and morphometrical characters can be generically attributed to archaic Homo sapiens. The lithic industry is formed by flakes, carinated points, scrapers, choppers and chopping tools and is characteristic of the Italian Pebble Culture. Sediments, pollen and faunal remains indicate that this part of the deposit was formed during interglacial climatic conditions in the early, but not initial phase of Middle Pleistocene (isotopic stadium 13 or 11).

PalynologyArcheologyPaleontologyGeographyPleistoceneHomo sapiensFaunaInterglacialSedimentologyPebbleArchaeologyChronology
researchProduct

Upper Pleistocene biostratigraphy and traces of glaciotectonics at the Satiki site, western Latvia

2007

Structural, lithological, palynological and plant macroremain investigations of test-boring cores and gravel pit walls at the Satiki site suggest that gyttja and sandy gyttja units of basin sediments were deposited during the Felicianova (Eemian) Interglacial. A pollen diagram reflects the characteristic forest succession of the Eemian Interglacial: Betula, Pinus, Ulmus, Corylus, Quercus, Fraxinus, Tilia, Carpinus, Picea and Pinus. Forests of broadleaved trees and thermophilous plants dominated in the surroundings of the lake during the interglacial climatic optimum. The basin sediments contain a large number of warmth-demanding water plants such as Salvinia natans and Trapa sp. Paleobotani…

PalynologyPaleontologyEemianInterglacialSedimentary rockBiostratigraphyWeichselian glaciationGeologyDevonianEarth-Surface ProcessesGyttjaQuaternary International
researchProduct

A Cromerian Complex palaeolake sediment sequence from the Zidini site, south-eastern Latvia

2013

Abstract This study is based upon palaeobotanical reinvestigation of the Pleistocene deposit strata revealed by test drillings in the buried valley at the Zidini site, southeastern Latvia. Up to 100 m thick lake sediment strata covered by three different till layers have been found in three 120–171 m deep test drillings. New palynological and plant macroremain analysis for sediment samples from core No. 43 have been done. These results and data from the earlier investigations at Zidini were compared. Clearer insights into depositional environment and vegetation change during the accumulation of sediments in the palaeolake have been acquired. According to recent studies and correlation of ob…

PalynologySedimentary depositional environmentSequence (geology)PaleontologyPleistoceneInterglacialSedimentGlacial periodStadialGeologyEarth-Surface ProcessesQuaternary International
researchProduct

27. A new holsteinian pollen record from the dry maar at Döttingen (Eifel)

2007

Abstract A new interglacial pollen sequence from the Dottingen dry maar in the Eifel region of the Rheinish Schield is presented. Palynology is used to correlate with several classical north German Holsteinian sites. The lake sediments reveal the complete interglacial and also 60 m of laminated sediments from the glacial preceding the Holsteinian. The interglacial section indicates limnic conditions in its lower part and telmatic conditions in its upper part with an intermediate episode of peat formation. Ash layers document intensive volcanism during the interglacial in the Eifel region. Some of the north German Holsteinian sites reveal spikes of high abundance of Pinus, Betula and Poaceae…

PalynologySequence (geology)PaleontologyPollenInterglacialmedicineGlacial periodVolcanismVegetationmedicine.disease_causeGeologyMaar
researchProduct

Orbital variations in planktonic foraminifera assemblages from the Ionian Sea during the Middle Pleistocene Transition

2013

Abstract The Middle Pleistocene Transition (1.2–0.7 Ma) is the most recent re-organization of the global climate system which includes variations in the frequency and amplitude of glacial/interglacial cycles, increased ice sheet volume, sea surface temperature cooling and a significant drop in the CO 2 atmospheric levels. Here we present high-resolution planktonic foraminifera data (mean sampling resolution of about 780 years) from core LC10 recovered in the Ionian Sea (eastern Mediterranean), between 1.2 and 0.9 Ma. Selected taxa, among them G. ruber , T. quinqueloba and G. bulloides , show significant periodicities that can be associated to orbital cycles, mainly precession and obliquity.…

Planktonic foraminifera010504 meteorology & atmospheric sciencesPleistoceneMiddle Pleistocene Transition010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaPaleontology14. Life underwaterGlacial periodEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyOrbital climate variabilitygeography.geographical_feature_categorybiologyPaleontologySapropelIonian SeaPlanktonic Foraminifera Eastern Mediterranean Middle Pleistocene transitionbiology.organism_classificationNeogloboquadrina pachyderma sinistral coilingSea surface temperatureOceanography13. Climate actionInterglacialIce sheetQuaternaryGeology
researchProduct

Cyclic fluctuations, climatic changes and role of noise in planktonic foraminifera in the Mediterranean Sea

2005

The study of Planktonic Foraminifera abundances permits to obtain climatic curves on the basis of percentage ratio between tropical and temperate/polar forms. Climatic changes were controlled by several phenomena as: (i) Milankovitch's cycles, produced by variations of astronomical parameters such as precession, obliquity and eccentricity; (ii) continental geodynamic evolution and orogenic belt; (iii) variations of atmospheric and oceanic currents; (iv) volcanic eruptions; (v) meteor impacts. But while astronomical parameters have a quasi-regular periodicity, the other phenomena can be considered as "noise signal" in natural systems. The interplay between cyclical astronomical variations, t…

Planktonic foraminiferaStochastic resonanceGeneral MathematicsGeneral Physics and AstronomyAtmospheric sciencesQuantitative Biology - Quantitative MethodsPhysics::GeophysicsForaminiferaMediterranean seaGlacial periodQuantitative Biology - Populations and EvolutionPlanktonic foraminifera; Climatic changes; Stochastic resonancePhysics::Atmospheric and Oceanic PhysicsQuantitative Methods (q-bio.QM)Milankovitch cyclesbiologyOcean currentPopulations and Evolution (q-bio.PE)biology.organism_classificationSettore FIS/07 - Fisica Applicata(Beni Culturali Ambientali Biol.e Medicin)Climatic changeOceanographyFOS: Biological sciencesInterglacialPrecessionAstrophysics::Earth and Planetary AstrophysicsGeologyStochastic resonance
researchProduct