2019FigshareOpen access

Holocene sea-surface reconstructions in Canadian Arctic

David Ledu

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Abstract

These are quantitative climate reconstruction from three marines cores retrieved in the main axis of the Northwest Passage, Canadian Arctic. These include reconstruction of sea-ice cover, sea-surface temperature and sea-surface salinity over the last 10 000 years. Quantitative reconstructions are based on dinoflagellate cyst assemblage.

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What this paper is about

These are quantitative climate reconstruction from three marines cores retrieved in the main axis of the Northwest Passage, Canadian Arctic. These include reconstruction of sea-ice cover, sea-surface temperature and sea-surface salinity over the last 10 000 years. Quantitative reconstructions are based on dinoflagellate cyst assemblage.

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Available abstract

These are quantitative climate reconstruction from three marines cores retrieved in the main axis of the Northwest Passage, Canadian Arctic. These include reconstruction of sea-ice cover, sea-surface temperature and sea-surface salinity over the last 10 000 years. Quantitative reconstructions are based on dinoflagellate cyst assemblage.

Key concepts: Holocene, Oceanography, Geology, Arctic, Physical geography, The arctic, Climatology, Geography

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