0000000000916232

AUTHOR

Jan Weckström

0000-0001-5604-617x

showing 2 related works from this author

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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Climate controls on the Holocene development of a subarctic lake in northern Fennoscandia

2015

International audience; Climate exerts strong control over the functioning of northern freshwater ecosystems, yet their resilience and responses to climate forcing may vary. We examined postglacial development patterns in subarctic Lake Varddoaijavri to discern the impact of direct climate controls, catchment influence, and ontogenic processes on the ecological functioning of the lake over the Holocene. Subfossil diatom assemblages together with the elemental and stable isotopic (delta C-13, delta N-15) composition of sediment organic matter were used to examine climate-induced changes in the structure of the phototrophic community and transport of terrestrial organic matter from the catchm…

ArcheologyHolocene climate[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]ta1171Freshwater ecosystemCarbon utilizationWater columnstable isotope14. Life underwaterEcology Evolution Behavior and SystematicsHoloceneOrganic carbonIsotope analysisStable isotopesSubarctic lakesDiatomsGlobal and Planetary ChangeSubfossilEcologyPaleohydrologyGeology15. Life on landCladoceraSubarctic climateFood web[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionEnvironmental scienceQuaternary Science Reviews
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