The signal of climate changes over the last two millennia in the Gulf of St. Lawrence, eastern Canada
Datos Bibliográficos
| ID | 24085657 |
|---|---|
| Autores | Xiner Wu (0000-0002-4072-392X, Université du Québec à Montréal, autor de correspondencia), Anne De Vernal (0000-0001-5656-724X, Université du Québec à Montréal), Bianca Fréchette (0000-0002-4986-5772, Université du Québec à Montréal), Matthias Moros (0000-0003-1061-0892, Leibniz Institute for Baltic Sea Research Warnemünde), Kerstin Perner (0000-0002-7464-2191, Leibniz Institute for Baltic Sea Research Warnemünde) |
| Año | 2022 |
| Volumen | 106 |
| Páginas | 28-43 |
| Fecha de publicación | 2022-03-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Quaternary Research (JOURNAL) |
| Identificadores de la revista | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editorial | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/qua.2021.56 |
| OpenAlex | W3211251005 |
| Idioma | EN |
| Citas recibidas | 3 |
| Referencias citadas | 53 |
Climate changes over the past two millennia in the central part of the Gulf of St. Lawrence are documented in this paper with the aim of determining and understanding the natural climate variability and the impact of anthropogenic forcing at a regional scale. The palynological content (dinocysts, pollen, and spores) of the composite marine sediment core MSM46-03 collected in the Laurentian Channel was used to reconstruct oceanographic and climatic changes with a multidecadal temporal resolution. Sea-surface conditions, including summer salinity and temperature, sea-ice cover, and primary productivity, were reconstructed from dinocyst assemblages. Results revealed a remarkable cooling trend of about 4°C after 1230 cal yr BP (720 CE) and a culmination with a cold pulse dated to 170–40 cal yr BP (1780–1910 CE), which likely corresponds to the regional signal of the Little Ice Age. This cold interval was followed by a rapid warming of about 3°C. In the pollen assemblages, the decrease of Pinus abundance over the past 1700 yr suggests changes in wind regimes, likely resulting from increased southerly incursions of cold and dry Arctic air masses into southeastern Canada.
Abrupt climate change · Alkenone · Arctic · Climate change · Climatology · Dinocyst · Effects of global warming · Geography · Global warming · Holocene · Palynology · Physical geography · Pollen · Ecology · Geology · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Marine and environmental studies · Oceanography
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Multi-proxy reconstruction of climate changes in the Lower St. Lawrence Estuary, Canada, during the Middle and Late-Holocene
High-resolution forest and fire dynamics from Fish Lake, New Brunswick, Canada, during the last millennium
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Climate, History And The Modern World
Dark Ages Cold Period
Late-Holocene sea-surface conditions offshore Newfoundland based on dinoflagellate cysts
Late-Holocene atmospheric dust deposition in eastern Canada (St. Lawrence North Shore)
IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP
| Obras citantes distintas | 3 |
|---|---|
| Citas por año | 0,75 |
| Intervalo de citas | 2022 - 2026 (5) |
| Velocidad de citación | current |
| Altamente citado | No |
| Tipos de cita | Neutras: 3 |