Search results for "Maxim"

showing 10 items of 1236 documents

Determination of water speciation in hydrous haplogranitic glasses with partial Raman spectra

2020

Abstract We use a mathematical approach to decompose the Raman water band at 3000 cm−1 to 3750 cm−1 into two partial Raman spectra corresponding to the individual Raman activity of the two water species, i.e., molecular water (H2Om) and OH-groups, present in hydrous rhyolitic glasses. The approach is based on a least-squares optimization algorithm and the assumption that the water band can be expressed as a linear combination of two partial Raman spectra. Our model makes no assumptions regarding the shape of the partial Raman spectra. The model input consists of about 700 Raman spectra from hydrous haplogranitic (HPG8) compositions with total water contents from 0.6 to 3.1 wt% and with know…

010504 meteorology & atmospheric sciencesOptimization algorithmmedia_common.quotation_subjectAnalytical chemistryInfrared spectroscopyGeology010502 geochemistry & geophysics01 natural sciencesSpeciationsymbols.namesakeGeochemistry and PetrologyYield (chemistry)symbolsMaximaRaman spectroscopyGeologyEquilibrium constant0105 earth and related environmental sciencesmedia_commonChemical Geology
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Holocene land-cover reconstructions for studies on land cover-climate feedbacks

2010

The major objectives of this paper are: (1) to review the pros and cons of the scenarios of past anthropogenic land cover change (ALCC) developed during the last ten years, (2) to discuss issues related to pollen-based reconstruction of the past land-cover and introduce a new method, REVEALS (Regional Estimates of VEgetation Abundance from Large Sites), to infer long-term records of past land-cover from pollen data, (3) to present a new project (LANDCLIM: LAND cover – CLIMate interactions in NW Europe during the Holocene) currently underway, and show preliminary results of REVEALS reconstructions of the regional land-cover in the Czech Republic for five selected time windows of the Holocene…

010504 meteorology & atmospheric sciencesStratigraphyREGIONAL VEGETATION01 natural sciencesAgricultural landAbundance (ecology)ddc:551new project LANDCLIMddc:550land-cover changelcsh:TD169-171.8GLACIAL-MAXIMUMHolocenelcsh:Environmental scienceslcsh:GE1-350ClimatologyGlobal and Planetary ChangeSOUTHERN SWEDENGeologyLast Glacial MaximumVegetation[SHS.GEO]Humanities and Social Sciences/GeographyPOLLEN-REPRESENTATIONClimatologyLANDCLIMlcsh:TD172-193.5GeologiTerrestrial ecosystemCARBON-CYCLEland cover-climate feedbacks010506 paleontology117 Geography Environmental scienceslcsh:Environmental protectioneducationAnnan geovetenskap och miljövetenskapLand coverLand cover changelcsh:Environmental pollutionREVEALSSIMULATION APPROACH0105 earth and related environmental sciencesEUROPEAN CLIMATEHolocenePaleontology15. Life on landQUANTITATIVE RECONSTRUCTIONPAST VEGETATIONNW EuropeTERRESTRIAL ECOSYSTEMSEarth sciences13. Climate actionPaleoecologyOther Earth and Related Environmental Sciences
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Topographic descriptors and thermal inversions amid the plateaus and mountains of the Jura (France)

2018

Sixteen temperature measurement sites under forest cover are distributed across the plateaus and mountains of the Jura (France). They are composed of pairs of stations located, one at the bottom of a topographic trough, the other at least 50 m higher in altitude. Three descriptors (station elevation, altitudinal difference (amplitude) between the two stations of each site, and topographical context) are used to explain how the frequency, intensity, and duration of inversions are spatially structured. Depending on whether one considers: 1) tn (minimum temperature) or tx (maximum temperature), 2) frequency or intensity, the sign of the correlation values changes. This reflects the fact that n…

010504 meteorology & atmospheric scienceselevation0208 environmental biotechnologyTopographie02 engineering and technology01 natural sciencesinversion[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologytopographyForest coverLinear regressionJura0105 earth and related environmental sciencesMaximum temperatureInversion (meteorology)General Medicine15. Life on landGeodesy020801 environmental engineeringAmplitudetempérature sous couvert forestier13. Climate actiontemperature under forest coverMaximaGeologyaltitude
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Productivity modes in the Mediterranean Sea during Dansgaard–Oeschger (20,000–70,000 yr ago) oscillations

2013

The study of planktonic organisms during abrupt climatic variations of the last glacial period (Dansgaard-Oeschger oscillations, D-O) may reveal important insights on climatic, oceanographic and biological interactions. Here we present planktic foraminifera and coccolithophore data collected at the Ocean Drilling Program Site 963 (Sicily Channel), with a mean sampling resolution of respectively 43.5 and 98.9. yr, over the interval between 70,000 and 20,000. yr ago. The paleoenvironmental reconstruction suggests that three different scenarios can be seen across each D-O cycle: 1. oligotrophic surface water and a deep thermocline for the early Interstadials; 2. a Deep Chlorophyll Maximum and …

010506 paleontology010504 meteorology & atmospheric sciencesCoccolithophoreMediterraneanOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnMediterranean seaPaleoproductivity Dansgaard–Oeschger Mediterranean Planktonic Foraminifera CoccolithophoresCoccolithophores14. Life underwaterStadialGlacial periodSDG 14 - Life Below WaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesDeep chlorophyll maximumbiologyPaleontologybiology.organism_classificationOceanography13. Climate actionClimatologyPlanktonic ForaminiferaDansgaard-OeschgerThermoclineGeologyPaleoproductivityPalaeogeography, Palaeoclimatology, Palaeoecology
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Large-scale, millennial-length temperature reconstructions from tree-rings

2018

Supported by the German Science Foundation, grants # Inst 247/665-1 FUGG and ES 161/9-1. SSG acknowledges support by the Alexander von Humboldt Foundation, KJA by US National Science Foundation grants AGS-1501856 and NSF AGS-1501834, and JL and LS by the Belmont Forum and JPI-Climate, Collaborative Research Action INTEGRATE. Over the past two decades, the dendroclimate community has produced various annually resolved, warm season temperature reconstructions for the extratropical Northern Hemisphere. Here we compare these tree-ring based reconstructions back to 831 CE and present a set of basic metrics to provide guidance for non-specialists on their interpretation and use. We specifically d…

010506 paleontology010504 meteorology & atmospheric sciencesNDASPlant ScienceWarm season01 natural sciencesG1Extratropical cycloneddc:550Little ice ageBeneficial effectsWarm season temperatures0105 earth and related environmental sciencesNorthern Hemisphereddc:333.7-333.9EcologyNorthern HemisphereG Geography (General)Medieval Warm PeriodCovarianceTree-ring widthMaximum latewood densityTree (data structure)ClimatologyLittle Ice AgeScale (map)Geology
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Summer air temperature, reconstructions from the last glacial stage based on rodents from the site Taillis-des-Coteaux (Vienne), Western France.

2014

AbstractThe oxygen isotope composition of phosphate from tooth enamel of rodents (δ18Op) constitutes a valuable proxy to reconstruct past air temperatures in continental environments. This method has been applied to rodent dental remains from three genera, Arvicola sp., Microtus sp. and Dicrostonyx sp., coming from Taillis-des-Coteaux, Vienne, France. This archaeological site contains an exceptionally preserved sedimentary sequence spanning almost the whole Upper Palaeolithic, including seven stratigraphic layers dated from 35 to 17 cal ka BP. The abundant presence of rodent remains offers the opportunity to quantify the climatic fluctuations coeval of the various stages of human occupation…

010506 paleontology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesClimatePhosphate01 natural sciencesIsotopes of oxygenPaleontologyArts and Humanities (miscellaneous)Late Pleistocene[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGlacial periodMicrotus0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRodentbiologyLast Glacial Maximum15. Life on landbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryOxygen isotopestomatognathic diseases[ SDE.MCG ] Environmental Sciences/Global ChangesAir temperatureArvicolaGeneral Earth and Planetary SciencesSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyHeterochronyGeology
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New tree-ring evidence for the Late Glacial period from the northern pre-Alps in eastern Switzerland

2018

Abstract The rate and magnitude of temperature variability at the transition from the Last Glacial Maximum into the early Holocene represents a natural analog to current and predicted climate change. A limited number of high-resolution proxy archives, however, challenges our understanding of environmental conditions during this period. Here, we present combined dendrochronological and radiocarbon evidence from 253 newly discovered subfossil pine stumps from Zurich, Switzerland. The individual trees reveal ages of 41–506 years and were growing between the Allerod and Preboreal (∼13′900–11′300 cal BP). Together with previously collected pines from this region, this world's best preserved Late…

010506 paleontologyArcheologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesGeologyLast Glacial Maximum01 natural scienceslaw.inventionAllerød oscillationGeographyPreboreal13. Climate actionlawDendrochronologyGlacial periodRadiocarbon datingYounger DryasPhysical geographyCentral Europe; Dendrochronology; Late Glacial; Paleoclimatology; Radiocarbon; Subfossil wood; Switzerland; Tree rings; Younger DryasEcology Evolution Behavior and SystematicsHolocene0105 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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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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