Search results for "PALEOCLIMATE RECONSTRUCTION"

showing 2 items of 2 documents

Comparison of quantitative Holocene temperature reconstructions using multiple proxies from a northern boreal lake

2017

Four biotic proxies (plant macrofossils, pollen, chironomids and diatoms) are employed to quantitatively reconstruct variations in mean July air temperatures ( Tjul) at Lake Loitsana (northern Finland) during the Holocene. The aim is to evaluate the robustness and biases in these temperature reconstructions and to compare the timing of highest Tjul in the individual reconstructions. The reconstructed Tjul values are evaluated in relation to local-scale/site-specific processes associated with the Holocene lake development at Loitsana as these factors have been shown to significantly influence the fossil assemblages found in the Lake Loitsana sediments. While pollen-based temperatures follow…

1171 GeosciencesInsolation010506 paleontologyArcheology010504 meteorology & atmospheric sciencesecological driversCLIMATE RECONSTRUCTIONSta1171CENTRAL NORWAYchironomidsWetlandEASTERN-EUROPEAN RUSSIANorthern finlandmedicine.disease_cause01 natural sciencesdiatomsPollenpiilevätmedicineTREE-LINE AREAsurviaissääsketplant macrofossils1172 Environmental sciencesHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologySUB-ARCTIC FINLANDPaleontologyMacrofossilFINNISH LAPLANDpaleolimnologiaBoreal13. Climate actionpollenClimatologyta1181paleoklimatologiaPALEOCLIMATE RECONSTRUCTIONSCHIRONOMIDAE INSECTAnorthern boreal FennoscandiaPhysical geographymakrofossiilitsiitepölyanalyysiGeologyThe Holocene
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A 5500-year oxygen isotope record of high arctic environmental change from southern Spitsbergen

2017

The oxygen isotope composition of chironomid head capsules in a sediment core spanning the past 5500 years from Lake Svartvatnet in southern Spitsbergen was used to reconstruct the oxygen isotope composition of lake water (δ18Olw) and local precipitation. The δ18Olw values display shifts from the baseline variability consistent with the timing of recognized historical climatic episodes, such as the Roman Warm Period, the Dark Ages Cold Period and the ‘Little Ice Age’. The highest values of the record, ca. 3‰ above modern δ18Olw values, occur at ca. 1900–1800 cal. yr BP. Three negative excursions increasing in intensity toward the present, at 3400–3200, 1250–1100, and 350–50 cal. yr BP, are…

TEMPERATURE VARIABILITY1171 GeosciencesSpitsbergen010506 paleontologyArcheology010504 meteorology & atmospheric sciencesEnvironmental change"Little Ice Age'NORTH-ATLANTIC CLIMATE01 natural sciencesIsotopes of oxygenSVALBARD ICE CORESvalbardArcticSea iceEAST GREENLAND CURRENTPrecipitationRoman Warm Periodclimate0105 earth and related environmental sciencesEarth-Surface Processes‘Little Ice Age’Global and Planetary ChangegeographyHOLOCENE GLACIER FLUCTUATIONSgeography.geographical_feature_categoryEcologyLATE-PLEISTOCENEoxygen isotopesBaseline (sea)LAKE-WATER DELTA-O-18North AtlanticPaleontologytemperatureGlacierPALEOCLIMATE RECONSTRUCTIONOceanographyArctic13. Climate actionta1181SEA-ICEGeologyHIGH-RESOLUTIONHolocene
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