A biological consequence of reducing Arctic ice cover: arrival of the Pacific diatom Neodenticula seminae in the North Atlantic for the first time in 800 000 years

By Philip C. Reid, D. Johns, M. Edwards, M. Starr, M. Poulin, P. Snoeijs. 2007

185 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/fe709d8171993af0843a6f46fc104114625a4f01

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Citations in the corpus

Marine range shifts and species introductions: comparative spread rates and community impacts (2010, background): “Additional species are likely to be poised for future range shifts, such as North Pacific Ocean species for which continued climate warming may allow migration through Arctic corridors into the North Atlantic Ocean (Reid et al., 2007; Vermeij & Roopnarine, 2008), as occurred during earlier Tertiary ”
Penetration of Pacific zooplankton into the western Arctic Ocean tracked with molecular population genetics (2009, background): “…between the Pacific and Arctic Oceans is thought to have opened approximately 5.32 million years ago (Gladenkov et al. 2002), making the Arctic Ocean a transit route for biotic exchange between the Atlantic and Pacific Oceans (Vermeij 1991, Lindstrom 2001, Nikula et al. 2007, Reid et al. 2007).”
Impacts of climate change on marine organisms and ecosystems. (2009, background): “Warming in the Arctic has enabled trans-polar invasion of the Atlantic by Pacific plankton species [108].”
The effects of climate change on species composition, succession and phenology: a case study (2011, background): “While climate change research has begun to document the effects of these two individual stressors on species and ecosystems (e.g., Gilman et al., 2006; Mieszkowska et al., 2006; Kirby et al., 2007; Reid et al., 2007; Beaugrand et al., 2010; Sorte et al., 2010a), few studies have evaluated the relati”
Australia's Biodiversity and Climate Change (2010, background): “2007), and marine species from the Atlantic Ocean flowing into the North Pacific Ocean via the Northwest Passage (Reid et al. 2007).”
Climate change impacts on marine ecosystems. (2012, background): “For example, the diatom Neodenticula seminae, a dominant primary producer in North Pacific pelagic ecosystems, became abundant in 1999 in the Atlantic for the first time in 800,000 years following an exceptional year of ice-free water in the Canadian Arctic (Reid et al. 2007).”
The pan-Arctic biodiversity of marine pelagic and sea-ice unicellular eukaryotes: a first-attempt assessment (2011, background): “…climate warming may explain the reappearance of the North Pacific plankton diatom, Neodenticula seminae (Simonsen & Kanaya) Akiba & Yanagisawa, in the North Atlantic through a pulse of Pacific water via the Canadian Arctic Archipelago and/or the Fram Strait (Poulin et al. 2010; Reid et al. 2007).”
Footprints of climate change in the Arctic marine ecosystem (2011, background): “During early postglacial periods the boreal species Mytilus edulis was established as far north as Spitsbergen, after which the species disappeared again (Berge et al., 2005).”
Biodiversity and phylogeography of Arctic marine fauna: insights from molecular tools (2011, background): “At least some of these new records may represent recent northward range expansions of boreal species (e.g., Johns et al. 2005; Fleischer et al. 2007; Reid et al. 2007; Sirenko and Gagaev 2007; Nelson et al. 2009), as predicted under a warming climate scenario (Vermeij and Roopnarine 2008).”
Phytoplankton niches estimated from field data (2012, background): “Important caveats are that the emergence of novel habitats, the introduction of invading phytoplankton or grazers, or mismatch between predators and prey (Edwards and Richardson 2004) could alter ecological niches and complicate future predictions (Edwards et al. 2001; Reid et al. 2007; Williams and”