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Hilary Kennedy

Researcher at Bangor University

Publications -  123
Citations -  7995

Hilary Kennedy is an academic researcher from Bangor University. The author has contributed to research in topics: Sea ice & Seagrass. The author has an hindex of 42, co-authored 117 publications receiving 6470 citations. Previous affiliations of Hilary Kennedy include UPRRP College of Natural Sciences & University of Cambridge.

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Ion microprobe assessment of the heterogeneity of Mg/Ca, Sr/Ca and Mn/Ca ratios in Pecten maximus and Mytilus edulis (bivalvia) shell calcite precipitated at constant temperature

TL;DR: In the mid and innermost regions of the P. maximus shell the lack of significant small-scale variation of Mg/Ca ratios, which is consistent with growth at constant temperature, suggest a potential application as a palaeotemperature proxy.
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Surface ice and gap layers in Antarctic sea ice: highly productive habitats

TL;DR: In this paper, the upper layers of sea ice were made on layered sum- mer ice floes collected from the Weddell Sea, Antarctica, from mid-February to March 1997.
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An ikaite record of late Holocene climate at the Antarctic Peninsula

TL;DR: In this paper, the first downcore δ 18 O record of natural ikaite hydration waters and crystals collected from the Antarctic Peninsula (AP) is reported, which qualitatively supports that both the Medieval Warm Period and Little Ice Age extended to the AP during the late Holocene.
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Biogeochemistry of platelet ice: its influence on particle flux under fast ice in the Weddell Sea, Antarctica

TL;DR: There was a substantial flux of particulate organic material out of the platelet layer, although higher amounts were collected in the traps either side of the thermocline, and the size classes of these pellets suggest they derive from protists grazing rather than from larger metazoans.
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Marine production in the Congo-influenced SE Atlantic over the past 30,000 years: A novel dinoflagellate-cyst based transfer function approach

TL;DR: In this article, the authors used modern analogues and a dinocyst transfer function to reconstruct primary palaeoproductivity (PP) in a region of freshwater influence.