GEOSCAN, résultats de la recherche


TitreClimate change and decadal to centennial-scale periodicities recorded in a late Holocene NE Pacific marine record: Examining the role of solar forcing
AuteurGalloway, J M; Wigston, A; Patterson, R T; Swindles, G T; Reinhardt, E; Roe, H M
SourcePalaeogeography, Palaeoclimatology, Palaeoecology vol. 386, 2013 p. 669-689,
Séries alt.Secteur des sciences de la Terre, Contribution externe 20110426
Documentpublication en série
Mediapapier; en ligne; numérique
SNRC92M/02; 92M/03; 92M/04
Lat/Long OENS-128.0000 -126.7500 51.2500 51.0000
SujetsHolocène; fluctuations climatiques; effets climatiques; diatomées; changements du niveau de la mer; variations du niveau de la mer; Changement climatique; paléontologie; sédimentologie; Cénozoïque
Illustrationslocation maps; plots; stratigraphic sections
Programmepipeline nordiques, Géoscience de l'environnement
Résumé(disponible en anglais seulement)
We present a decadal-scale late Holocene climate record based on diatoms, biogenic silica, and grain size from a 12-m sediment core (VEC02A04) obtained from Frederick Sound in the Seymour-Belize Inlet Complex of British Columbia, Canada. Sediments are characterized by graded, massive, and laminated intervals. Laminated intervals are most common between c. 2948-2708 cal. yr BP and c. 1992-1727 cal. yr BP. Increased preservation of laminated sediments and diatom assemblage changes at this time suggest that climate became moderately drier and cooler relative to the preceding and succeeding intervals. Spectral and wavelet analyses are used to test for statistically significant periodicities in time series of proxies of primary production (total diatom abundance, biogenic silica) and hydrology (grain size) preserved in the Frederick Sound record. Periodicities of c. 42-53, 60-70, 82-89, 241-243, and 380 yrs are present. Results are compared to reconstructed sunspot number data of Solanki et al. (2004) using cross wavelet transform to evaluate the role of solar forcing on NE Pacific climate. Significant common power of periodicities between c. 42-60, 70-89, 241-243, and of 380 yrs occur, suggesting that celestial forcing impacted late Holocene climate at Frederick Sound. Replication of the c. 241-243 yr periodicity in sunspot time series is most pronounced between c. 2900 cal. yr BP and c. 2000 cal. yr BP, broadly correlative to the timing of maximum preservation of laminated sedimentary successions and diatom assemblage changes. High solar activity at the Suess/de Vries band may have been manifested as a prolonged westward shift and/or weakening of the Aleutian Low in the mid-late Holocene, which would have diverted fewer North Pacific storms and resulted in the relatively dry conditions reconstructed for the Seymour-Belize Inlet Complex.