Search results for "SYSTEMATICS"

showing 10 items of 6702 documents

Improving the accuracy of small vertebrate-based palaeoclimatic reconstructions derived from the Mutual Ecogeographic Range. A case study using geogr…

2019

Abstract Understanding past climate and the mechanisms of climate change remain major challenges in scientific research. The Mutual Ecogeographic Range (MER) method for climatic reconstruction uses the current geographical distribution of fossil assemblages to infer palaeoclimatic conditions. Current species distributions used in the MER method are usually obtained from biogeographic atlases that record the absence/presence of species in a 10 × 10 km grid. A 10 × 10 km area is quite broad and the method only records presence/absence, without considering the real area occupied by any given species. Thus, the method overlooks the fact that environmental heterogeneity is strongly related to to…

010506 paleontologyArcheologyGlobal and Planetary ChangeGeographic information system010504 meteorology & atmospheric sciencesbiologyRange (biology)business.industryClimate changeVertebrateDistribution (economics)Geology01 natural sciencesbiology.animalPaleoclimatologyAssemblage (archaeology)Physical geographybusinessEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesQuaternary Science Reviews
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Vegetation and climate record from Abric Romaní (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)

2019

This study addresses the pollen record of Abric Romani archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of A…

010506 paleontologyArcheologyGlobal and Planetary ChangegeographyHumid continental climategeography.geographical_feature_category010504 meteorology & atmospheric sciencesPleistoceneSteppeGeologyVegetation01 natural sciencesInterglacialPaleoclimatologyPhysical geographyGlacial periodStadialEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesQuaternary Science Reviews
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Turia river delta and coastal barrier-lagoon of Valencia (Mediterranean coast of Spain): Geomorphological processes and global climate fluctuations s…

2019

Abstract Extensive drillings and 31 new C-14 datings were used to establish the geomorphological evolution of the Turia river delta and coastal barrier-lagoon system of Valencia (Spain) over the last three millennia. Integration of geomorphological, stratigraphic, malacological, sedimentological and geoarchaeological data enables us to relate river Turia avulsions and alluvial episodes to the development of coastal spits and barriers. Geomorphological changes in the study area may also be associated with global climate events, sea-level fluctuations or anthropogenic periods in the Turia catchment. Six phases may be differentiated: (1) a major early alluviation phase during the Iberian perio…

010506 paleontologyArcheologyGlobal and Planetary ChangegeographyRiver deltageography.geographical_feature_category010504 meteorology & atmospheric sciencesCoastal plainGeologyCoastal geography01 natural sciencesPaleoclimatologyBeach ridgeAlluviumPhysical geographyProgradationEcology Evolution Behavior and SystematicsHoloceneGeology0105 earth and related environmental sciencesQuaternary Science Reviews
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Caribbean hydroclimate and vegetation history across the last glacial period

2019

Abstract We present a new speleothem trace element and stable isotope record, which extends previous paleoclimate evidence from Cuban speleothems to the last 96 ka. Multiple proxies were used to reconstruct Caribbean hydroclimate and vegetation variability on orbital to millennial timescales. In particular, our proxies indicate a shift to more abundant C4 (compared to C3) vegetation and/or reduced soil activity during the Last Glacial Maximum. Our results confirm the close link of Caribbean precipitation to North Atlantic climate variability, insolation and the strength of the AMOC. The associated variations in Caribbean SSTs and the shift of the ITCZ led to substantial changes of the hydro…

010506 paleontologyArcheologyGlobal and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesSpeleothemGeologyLast Glacial Maximum01 natural sciencesAllerød oscillationPaleoclimatologyGlacial periodStadialPhysical geographyYounger DryasEcology Evolution Behavior and SystematicsGeologyHolocene0105 earth and related environmental sciencesQuaternary Science Reviews
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Hydroclimate variability of western Thailand during the last 1400 years

2020

Mainland Southeast Asia is located on the moisture transport route of the Indian summer monsoon (ISM) where hydroclimate records from speleothems have rarely been investigated. Here, we present a new multi-proxy (δ18O and δ13C values, trace element concentrations, and grayscale values) data set of stalagmite KPC1 from Khao Prae cave in western Thailand spanning the last 1400 years (500–1900 CE; the Common Era). These multi-proxy data reveal a high variability between the wet and dry periods during 500–850 CE and 1150–1300 CE, stable climate conditions during 850–1150 CE, and overall dry conditions since 1300 CE. The δ13C values, trace elements concentrations, and grayscale values show cente…

010506 paleontologyArcheologyGlobal and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ13Cδ18OSpeleothemGeologyStalagmite:Geology [Science]ThailandMonsoonSoutheast asianStalagmite01 natural sciencesPeriod (geology)MainlandPhysical geographyEcology Evolution Behavior and Systematics0105 earth and related environmental sciences
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Human occupation and environmental change in the western Maghreb during the Last Glacial Maximum (LGM) and the Late Glacial. New evidence from the Ib…

2019

With the onset of the Last Glacial Maximum (LGM), hunter-gatherers of the so-called Iberomaurusian techno-complex appeared in what is now the Mediterranean Maghreb. During a period of about seven thousand years, these groups left sandy occupation layers in a limited number of archaeological sites, while at the beginning of Greenland Interstadial (GI) 1, the sudden shift towards the deposition of shell-rich sediments and the increase in number of sites document clear changes in subsistence strategies as well as occupation density. It is highly likely that these shifts in human behaviour are related to paleoenvironmental changes in the area, which, so far, are poorly documented in geological …

010506 paleontologyArcheologyIfri El Baroud010504 meteorology & atmospheric sciencesEnvironmental changePalaeoenvironment01 natural sciencesVegetation dynamicsCaveLate PleistoceneGlacial periodStadialSedimentologyIberomaurusianGeoarchaeologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeoarchaeologyGeologyLast Glacial Maximum15. Life on landArchaeologyMorocco13. Climate actionIberomaurusian
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Paleogenetic and morphometric analysis of a Mesolithic individual from Grotta d'Oriente: An oldest genetic legacy for the first modern humans in Sici…

2020

Abstract Grotta d’Oriente, a coastal cave located on the island of Favignana (Sicily, Italy) is a key site for the study of the early human colonization of Sicily. Inside the cave, during different field excavations, three burials attributable to the Late Upper Palaeolithic and Mesolithic were found. The Mesolithic Oriente B individual, directly dated at 9,377 ± 25 uncal BP, was previously assigned to HV1 haplogroup using a traditional approach. However, it is well known that PCR based methods are prone to erroneous haplotype or haplogroup determination. In order to redefine the mitochondrial lineage of this Mesolithic hunter-gatherer and explore its phylogenetic position, we target-enriche…

010506 paleontologyArcheologyLineage (genetic)010504 meteorology & atmospheric sciencesMesolithic hunter-gatherersSettore BIO/08 - Antropologia01 natural sciencesHaplogroupCaveMorphometric analysisSicilyEcology Evolution Behavior and SystematicsMesolithic0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryAncient DNAHaplotypeGeologyLast Glacial MaximumArchaeologylanguage.human_languageGrotta d'OrienteAncient DNAlanguageSicilian
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Late Quaternary coastal uplift of southwestern Sicily, central Mediterranean sea

2021

Abstract Mapping and luminescence aging of raised marine terraces and aeolian ridges along an ∼90 km coastal stretch in southwestern Sicily provide the first quantitative assessment of vertical tectonic deformation in this region, which spans the frontal part of an active thrust belt. We recognized a staircase of eleven terraces and nine related aeolian ridges. The elevation profile of terraces parallel to the coast shows a >90 km long bell-shaped pattern, onto which shorter-wavelength (∼10 km long) undulations are superimposed. Luminescence ages from terraced beach deposits and aeolian sediments constrain the position of paleoshorelines formed during MIS 5e, 7a and 7c, with a maximum uplif…

010506 paleontologyArcheologyMarine terracesEarly Pleistocene010504 meteorology & atmospheric sciencesPleistoceneLuminescence datingSettore GEO/03 - Geologia StrutturaleFold growth01 natural sciencesMarine terracePaleontologyMediterranean seaContinental marginAeolian ridgeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangegeographyFrontal thrust beltgeography.geographical_feature_categoryThermoluminescence datingBedrockGeologyPleistoceneMediterranean seaAeolian ridgesAeolian processesQuaternaryGeologySouthwestern sicilyQuaternary Science Reviews
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Climate, environment and human behaviour in the Middle Palaeolithic of Abrigo de la Quebrada (Valencia, Spain): The evidence from charred plant and m…

2019

Abstract The Abrigo de la Quebrada rock shelter was occupied by Neanderthal groups during the early Upper Pleistocene, yielding evidence for their subsistence practices and local resource exploitation. This paper focuses on the plant macroremains and the micromammals, which provide information about occupation patterns, the surrounding landscape, the use of resources, and the environment. Mountain pine forests and permanent grass formations containing humid zones and open spaces that would have harboured an eurythermal microfauna were the dominant landscape type. Cold-climate pines provided most of the firewood. The data are consistent with a recurrent, seasonal occupation pattern, in which…

010506 paleontologyArcheologyNeanderthalTaphonomy010504 meteorology & atmospheric sciencesPleistoceneMicromammalsContext (language use)Firewood01 natural sciencesNeanderthalbiology.animalEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangebiologySubsistence agricultureGeologyArchaeologyGeographyAbrigo de la Quebrada (Valencia Spain)MicrofaunaCharcoalTaphonomySeedsWoodland exploitationRock shelter
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Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland

2016

Abstract: The developmental history, from the Oldest Dryas to the Late Holocene, of a paleolake and mire located in a river valley in Central Poland was studied using high-resolution records of pollen, macrofossils, Cladocera, sedimentology, and geochemistry from a 14 C dated sediment core. We inferred temperature and water level dynamics using cladocerans and palynological and geochemical methods were employed to investigate natural fluvial activity, particularly for these elements that are difficult to find through sedimentological methods. Our research demonstrates how climate fluctuation in the Late Glacial and Holocene periods influenced the development of a paleolake and mire in a sma…

010506 paleontologyArcheologyOldest Dryasta1171010502 geochemistry & geophysics01 natural sciencesAllerød oscillationPaleontologyIce corePaleoclimatologypaleoclimateYounger DryasGlacial periodEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary ChangeHoloceneMacrofossilGeology15. Life on landCladoceraLate Glacial13. Climate actionmultiproxy analysisPhysical geographyGeologyQuaternary Science Reviews
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