Search Results - "Naish, T"
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Choosing the future of Antarctica
Published in Nature (London) (01-06-2018)“…We present two narratives on the future of Antarctica and the Southern Ocean, from the perspective of an observer looking back from 2070. In the first…”
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The amplitude and origin of sea-level variability during the Pliocene epoch
Published in Nature (London) (01-10-2019)“…Earth is heading towards a climate that last existed more than three million years ago (Ma) during the ‘mid-Pliocene warm period’ 1 , when atmospheric carbon…”
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The multi-millennial Antarctic commitment to future sea-level rise
Published in Nature (London) (15-10-2015)“…Despite computational and methodological uncertainties, and a wide range of potential greenhouse gas emissions, here millennial-scale simulations of the…”
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East Antarctic ice sheet most vulnerable to Weddell Sea warming
Published in Geophysical research letters (16-03-2017)“…Models predict considerable spatial variability in the magnitude of future climate change around Antarctica, suggesting that some sectors of the continent may…”
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Antarctic ice-sheet sensitivity to obliquity forcing enhanced through ocean connections
Published in Nature geoscience (01-02-2019)“…Deep sea geological records indicate that Antarctic ice-sheet growth and decay is strongly influenced by the Earth’s astronomical variations (known as…”
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Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene
Published in Nature geoscience (01-11-2014)“…The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a transition from a global climate state that was 2–3 °C warmer than present…”
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Antarctic Cenozoic climate history from sedimentary records: ANDRILL and beyond
Published in Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences (28-01-2016)“…Mounting evidence from models and geological data implies that the Antarctic Ice Sheet may behave in an unstable manner and retreat rapidly in response to a…”
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Climatic and tectonic drivers of late Oligocene Antarctic ice volume
Published in Nature geoscience (01-10-2022)“…Cenozoic evolution of the Antarctic ice sheets is thought to be driven primarily by long-term changes in radiative forcing, but the tectonic evolution of…”
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Obliquity-paced Pliocene West Antarctic ice sheet oscillations
Published in Nature (19-03-2009)“…Thirty years after oxygen isotope records from microfossils deposited in ocean sediments confirmed the hypothesis that variations in the Earth's orbital…”
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Author Correction: Choosing the future of Antarctica
Published in Nature (London) (01-10-2018)“…On page 234 of this Perspective, ‘50% decrease’ has been corrected online to ‘50% increase’ in the sentence “The pH of surface waters south of 60° S decreased…”
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The Significance of Interseismic Vertical Land Movement at Convergent Plate Boundaries in Probabilistic Sea‐Level Projections for AR6 Scenarios: The New Zealand Case
Published in Earth's future (01-06-2024)“…Anticipating and managing the impacts of sea‐level rise for nations astride active tectonic margins requires understanding of rates of sea surface elevation…”
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Uncertain Pathways to a Future Safe Climate
Published in Earth's future (01-06-2024)“…Global climate change is often thought of as a steady and approximately predictable physical response to increasing forcings, which then requires commensurate…”
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Retreat of the Antarctic Ice Sheet During the Last Interglaciation and Implications for Future Change
Published in Geophysical research letters (16-09-2021)“…The Antarctic Ice Sheet (AIS) response to past warming consistent with the 1.5–2°C “safe limit” of the United Nations Paris Agreement is currently not well…”
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Bacterial abundance and composition in marine sediments beneath the Ross Ice Shelf, Antarctica
Published in Geobiology (01-07-2013)“…Marine sediments of the Ross Sea, Antarctica, harbor microbial communities that play a significant role in the decomposition, mineralization, and recycling of…”
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Retreat history of the Ross Ice Sheet (Shelf) since the Last Glacial Maximum from deep-basin sediment cores around Ross Island
Published in Palaeogeography, palaeoclimatology, palaeoecology (07-04-2008)“…Radiocarbon-dated sediment cores from deep basins beneath the McMurdo Ice Shelf, and seasonally open water north of Ross Island, McMurdo Sound, display a…”
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A Southwest Pacific Perspective on Long‐Term Global Trends in Pliocene‐Pleistocene Stable Isotope Records
Published in Paleoceanography and paleoclimatology (01-07-2018)“…Continuous stable isotope records from marine sediment cores spanning the Pliocene have been used to assess the oceans' response to major perturbations in the…”
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Constraining the amplitude of late Oligocene bathymetric changes in Western Ross Sea during orbitally-induced oscillations in the East Antarctic Ice Sheet: (1) Implications for glacimarine sequence stratigraphic models
Published in Palaeogeography, palaeoclimatology, palaeoecology (07-04-2008)“…Late Oligocene shallow glacimarine sequences recovered from western Ross Sea, Antarctica by the Cape Roberts (drilling) Project display orbitally-influenced…”
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Seismic stratigraphy of the Plio-Pleistocene Ross Island flexural moat-fill: a prognosis for ANDRILL Program drilling beneath McMurdo-Ross Ice Shelf
Published in Global and planetary change (01-02-2005)“…Ross Island volcanic complex began forming with the emplacement of the basaltic shield volcanoes of Mt. Bird and Mt. Terror between ca. 4.6 and 1.3 Ma, though…”
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Silicic tephras in Pleistocene shallow-marine sediments of Wanganui Basin, New Zealand
Published in Journal of the Royal Society of New Zealand (01-03-2005)“…Vitric-rich volcaniclastic horizons are important for correlation of glacio-eustatic sedimentary cycles, both within the well known shallow-marine record of…”
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Orbitally-influenced vegetation record of the Mid-Pleistocene Climate Transition, offshore eastern New Zealand (ODP Leg 181, Site 1123)
Published in Marine geology (30-04-2004)“…A census of Plio–Pleistocene (5–0 Ma) terrestrial palynomorph assemblages from ODP Site 1123, located 1100 km offshore eastern New Zealand and in a water depth…”
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