Stacking of discontinuous regional palaeoclimate records: Chironomid-based summer temperatures from the Alpine region

Autor: Laurent Millet, Boris P. Ilyashuk, Oliver Heiri, Stéphanie Samartin, André F. Lotter
Přispěvatelé: Laboratoire Chrono-environnement ( LCE ), Université Bourgogne Franche-Comté ( UBFC ) -Université de Franche-Comté ( UFC ) -Centre National de la Recherche Scientifique ( CNRS ), Oeschger Centre for Climate Change Research ( OCCR ), University of Bern, Palaeoecology, Institute of Environmental Biology, Utrecht University [Utrecht], Laboratoire Chrono-environnement - CNRS - UBFC (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Oeschger Centre for Climate Change Research (OCCR)
Jazyk: angličtina
Rok vydání: 2015
Předmět:
Zdroj: Holocene
Holocene, SAGE Publications, 2015, 25 (1), pp.137-149. 〈10.1177/0959683614556382〉
The Holocene
The Holocene, London: Sage, 2015, 25 (1), pp.137-149. ⟨10.1177/0959683614556382⟩
ISSN: 0959-6836
1477-0911
DOI: 10.1177/0959683614556382〉
Popis: Since multi-site reconstructions are less affected by site-specific climatic effects and artefacts, regional palaeotemperature reconstructions based on a number of sites can provide more robust estimates of centennial- to millennial-scale temperature trends than individual, site-specific records. Furthermore, reconstructions based on multiple records are necessary for developing continuous climate records over time scales longer than covered by individual sequences. Here, we present a procedure for developing such reconstructions based on relatively short (centuries to millennia), discontinuously sampled records as are typically developed when using biotic proxies in lake sediments for temperature reconstruction. The approach includes an altitudinal correction of temperatures, an interpolation of individual records to equal time intervals, a stacking procedure for sections of the interval of interest that have the same records available, as well as a splicing procedure to link the individual stacked records into a continuous reconstruction. Variations in the final, stacked and spliced reconstruction are driven by variations in the individual records, whereas the absolute temperature values are determined by the stacked segment based on the largest number of records. With numerical simulations based on the NGRIP δ18O record, we demonstrate that the interpolation and stacking procedure provides an approximation of a smoothed palaeoclimate record if based on a sufficient number of discontinuously sampled records. Finally, we provide an example of a stacked and spliced palaeotemperature reconstruction 15000–90 calibrated 14C yr BP based on six chironomid records from the northern and central Swiss Alps and eastern France to discuss the potential and limitations of this approach.
Databáze: OpenAIRE
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