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Sedimentary challenge to Snowball Earth
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instance of
scholarly article
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title
Sedimentary challenge to Snowball Earth
(English)
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main subject
Snowball Earth
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author name string
Philip A. Allen
series ordinal
1
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James L. Etienne
series ordinal
2
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language of work or name
English
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publication date
30 November 2008
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published in
Nature Geoscience
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volume
1
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issue
12
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page(s)
817-825
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exact match
https://scigraph.springernature.com/pub.10.1038/ngeo355
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cites work
Proterozoic (pre-Ediacaran) glaciation and the high obliquity, low-latitude ice, strong seasonality (HOLIST) hypothesis: Principles and tests
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Earth's glacial record and its tectonic setting
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A neoproterozoic snowball earth
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The snowball Earth hypothesis: testing the limits of global change
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Low palaeolatitude of deposition for late Precambrian periglacial varvites in South Australia: implications for palaeoclimatology
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The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South Australia
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Paleomagnetic polarity reversals in Marinoan (ca. 600 Ma) glacial deposits of Australia: Implications for the duration of low-latitude glaciation in Neoproterozoic time
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Stratigraphic, geochronological, and paleomagnetic constraints upon the Neoproterozoic climatic paradox
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The reliability of paleomagnetic data
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‘Zipper-rift’: a tectonic model for Neoproterozoic glaciations during the breakup of Rodinia after 750 Ma
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Glacio-epochs and the supercontinent cycle after ∼3.0 Ga: Tectonic boundary conditions for glaciation
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PALEOCLIMATE: An Appealing Snowball Earth That's Still Hard to Swallow
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Snowball Earth on trial
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Neoproterozoic glaciation in the Earth System
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Scenario for the evolution of atmospheric pCO2 during a snowball Earth
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Climate forcings and the initiation of low-latitude ice sheets during the Neoproterozoic Varanger glacial interval
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Neoproterozoic 'snowball Earth' simulations with a coupled climate/ice-sheet model
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CO2levels required for deglaciation of a “near-snowball” Earth
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Is there a conflict between the Neoproterozoic glacial deposits and the snowball Earth interpretation: an improved understanding with numerical modeling
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High levels of atmospheric carbon dioxide necessary for the termination of global glaciation
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Climate dynamics of a hard snowball Earth
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Investigating plausible mechanisms to trigger a deglaciation from a hard snowball Earth
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Snowball Earth prevention by dissolved organic carbon remineralization
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A snowball Earth versus a slushball Earth: Results from Neoproterozoic climate modeling sensitivity experiments
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GCM sensitivity test using increased rotation rate, reduced solar forcing and orography to examine low latitude glaciation in the neoproterozoic
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Low-latitude glaciation and rapid changes in the Earth's obliquity explained by obliquity-oblateness feedback
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Global climate model high-obliquity solutions to the ancient climate puzzles of the Faint-Young Sun Paradox and low-altitude Proterozoic glaciation
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Is high obliquity a plausible cause for Neoproterozoic glaciations?
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A 'snowball Earth' climate triggered by continental break-up through changes in runoff
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Coupled modeling of global carbon cycle and climate in the Neoproterozoic: links between Rodinia breakup and major glaciations
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Absence of a runaway ice-albedo feedback in the Neoproterozoic
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The impact of atmospheric and oceanic heat transports on the sea-ice-albedo instability during the Neoproterozoic
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Testing paleogeographic controls on a Neoproterozoic snowball Earth
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Glacial flow of floating marine ice in “Snowball Earth”
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Late Precambrian mixites: Glacial and/or nonglacial?
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7 January 2021
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Neoproterozoic glacial-rainout intervals: Observations and implications
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7 January 2021
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Precambrian permafrost horizons as indicators of palaeoclimate
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Subglacial and proglacial glacitectonic deformation in the Neoproterozoic Port Askaig Formation, Scotland
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Compositional and mineralogical variations in a Neoproterozoic glacially influenced succession, Mirbat area, south Oman: Implications for paleoweathering conditions
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Climatic cycles during a Neoproterozoic “snowball” glacial epoch
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An exceptionally thick upper Proterozoic (Sturtian) glacial succession in the Mount Painter area, South Australia
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Neoproterozoic snowball Earth under scrutiny: Evidence from the Fiq glaciation of Oman
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A record of Antarctic climate and ice sheet history recovered
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Geochronologic constraints on the chronostratigraphic framework of the Neoproterozoic Huqf Supergroup, Sultanate of Oman
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Glacial and syntectonic sedimentation: The upper Proterozoic Kingston Peak Formation, southern Panamint Range, eastern California
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Depositional controls on glacial facies associations in a basinal setting, late proterozoic, amadeus basin, Central Australia
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The role of subglacial water in ice-sheet mass balance
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U-Pb zircon date from the Neoproterozoic Ghaub Formation, Namibia: Constraints on Marinoan glaciation
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28th DeBeers Alex. Du Toit Memorial Lecture, 2004. On Cryogenian (Neoproterozoic) ice-sheet dynamics and the limitations of the glacial sedimentary record
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Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous?
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Detrital remanent magnetization in haematite-bearing Neoproterozoic Puga cap dolostone, Amazon craton: a rock magnetic and SEM study
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The age of the Nantuo Formation and Nantuo glaciation in South China
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Two or four Neoproterozoic glaciations?
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Isotopic compositions of carbonates and organic carbon from upper Proterozoic successions in Namibia: stratigraphic variation and the effects of diagenesis and metamorphism
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The Vendian succession of northeastern Spitsbergen: Petrogenesis of a dolomite-tillite association
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Secular variation in carbon isotope ratios from Upper Proterozoic successions of Svalbard and East Greenland
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Glacially-influenced deep-marine sedimentation of the Late Precambrian Gaskiers Formation, Newfoundland, Canada
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Toward a Neoproterozoic composite carbon-isotope record
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Constraints on the timing of Marinoan “Snowball Earth” glaciation by 187Re–187Os dating of a Neoproterozoic, post-glacial black shale in Western Canada
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Re-Os geochronology of postglacial black shales in Australia: Constraints on the timing of “Sturtian” glaciation
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U–Pb ages from the neoproterozoic Doushantuo Formation, China
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Near-synchronous interhemispheric termination of the last glacial maximum in mid-latitudes
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Are Proterozoic cap carbonates and isotopic excursions a record of gas hydrate destabilization following Earth's coldest intervals?
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Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates
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Carbon isotope evidence for widespread methane seeps in the ca. 635 Ma Doushantuo cap carbonate in south China
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Snowball Earth termination by destabilization of equatorial permafrost methane clathrate
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Extreme winds and waves in the aftermath of a Neoproterozoic glaciation
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Anomalous cold in the Pangaean tropics
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Carbonate deposition, climate stability, and Neoproterozoic ice ages
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Dynamics of the Neoproterozoic carbon cycle
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The Richtersveld Igneous Complex, South Africa: U‐Pb Zircon and Geochemical Evidence for the Beginning of Neoproterozoic Continental Breakup
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Direct dating of the Sete Lagoas cap carbonate (Bambuí Group, Brazil) and implications for the Neoproterozoic glacial events
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New U-Pb zircon dates for the Neoproterozoic Ghubrah glaciation and for the top of the Huqf Supergroup, Oman
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SHRIMP U-Pb geochronology of Neoproterozoic Windermere Supergroup, central Idaho: Implications for rifting of western Laurentia and synchroneity of Sturtian glacial deposits
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U-Pb SHRIMP ages of Neoproterozoic (Sturtian) glaciogenic Pocatello Formation, southeastern Idaho
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New constraints on the ages of Neoproterozoic glaciations in south China
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Identifiers
DOI
10.1038/NGEO355
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ADS bibcode
2008NatGe...1..817A
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Dimensions Publication ID
1000822464
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ResearchGate publication ID
248828221
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