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Lionel Carter

Researcher at Victoria University of Wellington

Publications -  172
Citations -  8099

Lionel Carter is an academic researcher from Victoria University of Wellington. The author has contributed to research in topics: Continental shelf & Terrigenous sediment. The author has an hindex of 52, co-authored 171 publications receiving 7358 citations. Previous affiliations of Lionel Carter include James Cook University & Indiana State University.

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Journal ArticleDOI

Coherent rainfall response to middle- and late-Holocene climate variability across the mid-latitude South Pacific

TL;DR: In the Southern Hemisphere mid-latitudes during the middle and late Holocene, a coherent pan-Pacific response to the growing influence that El Nino-Southern Oscillation (ENSO) and multicentury variations in the interaction between ENSO and the Southern Annular Mode (SAM) exerted on rainfall in New Zealand, Chile and Argentina as mentioned in this paper.
Journal ArticleDOI

New magnetobiostratigraphic chronology and paleoceanographic changes across the Oligocene-Miocene boundary at DSDP Site 516 (Rio Grande Rise, SW Atlantic)

TL;DR: In this paper, the authors used magnetobiostratigraphic data for the late Oligocene through early Miocene at the Deep Sea Drilling Project (DSDP) Hole 516F to provide a significantly revised age model, which permits reevaluation of developments that led to the Mi-1 glacial event at the oligocene-Miocene boundary.
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A budget for modern-Holocene sediment on the South Otago continental shelf

TL;DR: In this article, a sediment budget for the South Otago continental shelf and coast, between Nugget Point and Otago Peninsula, reveals modern (post 6500 y) sediment input is dominated by the Clutha River (total 3.14 Mt y−1; Mt = 106 tonnes).
Book ChapterDOI

Lower Circumpolar Deep Water Flow Through the SW Pacific Gateway for the Last 190 Ky: Evidence from Antarctic Diatoms

TL;DR: In this paper, tracer diatoms in cores located within the palaeo-LCDW flow-path may provide information on the flow of LCDW through the gateway for the last 190 ky, while that formed over the shelf is relatively enhanced in warmer times.