Regional atmospheric circulation change in the North Pacific during the Holocene inferred from lacustrine carbonate oxygen isotopes, Yukon Territory, Canada

Dados Bibliográficos

ID24086743
AutoresLesleigh Anderson (0000-0002-5264-089X, University of Massachusetts Amherst, autor correspondente), Mark B Abbott (0000-0002-0299-928X, Planetary Science Institute, autor correspondente), B Finney (0000-0002-2639-6512, University of Alaska Fairbanks, autor correspondente), Bruce P Finney, Stephen J Burns, Stephen Burns (0000-0003-4623-5326, University of Massachusetts Amherst, autor correspondente)
Ano2005
Volume64
Fascículo1
Páginas21-35
Data de publicação2005-07-01
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoQuaternary Research (JOURNAL)
Identificadores do periódicoISSN: 0033-5894 • E-ISSN: 1096-0287
EditoraCambridge University Press (CUP) (PUBLISHER)
DOI10.1016/j.yqres.2005.03.005
OpenAlexW1979287911
IdiomaEN
Citações recebidas28
Referências citadas64

Analyses of sediment cores from Jellybean Lake, a small, evaporation-insensitive groundwater-fed lake, provide a record of changes in North Pacific atmospheric circulation for the last ∽7500 yr at 5- to 30-yr resolution. Isotope hydrology data from the southern Yukon indicate that the oxygen isotope composition of water from Jellybean Lake reflects the composition of mean-annual precipitation, δ 18 O p . Recent changes in the δ 18 O of Jellybean sedimentary calcite (δ 18 O ca ) correspond to changes in the North Pacific Index (NPI), a measure of the intensity and position of the Aleutian Low (AL) pressure system. This suggests that δ 18 O p variability was related to the degree of fractionation during moisture transport from the Gulf of Alaska across the St. Elias Mountains and that Holocene shifts were controlled by the intensity and position of the AL. Following this model, between ∽7500 and 4500 cal yr B.P., long-term trends suggest a predominantly weaker and/or westward AL. Between ∽4500 and 3000 cal yr B.P. the AL shifted eastward or intensified before shifting westward or weakening between ∽3000 and 2000 cal yr B.P. Rapid shifts eastward and/or intensification occurred ∽1200 and 300 cal yr B.P. Holocene changes in North Pacific atmospheric circulation inferred from Jellybean Lake oxygen isotopes correspond with late Holocene glacial advances in the St. Elias Mountains, changes in North Pacific salmon abundance, and shifts in atmospheric circulation over the Beaufort Sea.

Atmospheric Circulation · Climatology · Geochemistry · Holocene · Isotopes of oxygen · Sedimentary rock · Climate change and permafrost · Geology · Geology and Paleoclimatology Research · Methane Hydrates and Related Phenomena · Oceanography · Paleontology