Hoffman, P. F. (1998) A Neoproterozoic Snowball Earth. Science, 281 (5381). 1342-1346 doi:10.1126/science.281.5381.1342
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | A Neoproterozoic Snowball Earth | ||
Journal | Science | ||
Authors | Hoffman, P. F. | Author | |
Year | 1998 (August 28) | Volume | 281 |
Page(s) | 1342-1346 | Issue | 5381 |
Publisher | American Association for the Advancement of Science (AAAS) | ||
DOI | doi:10.1126/science.281.5381.1342Search in ResearchGate | ||
Mindat Ref. ID | 2501028 | Long-form Identifier | mindat:1:5:2501028:0 |
GUID | 0f8e90cb-8105-4551-bce4-ddbdd1ba7f3b | ||
Full Reference | Hoffman, P. F. (1998) A Neoproterozoic Snowball Earth. Science, 281 (5381). 1342-1346 doi:10.1126/science.281.5381.1342 | ||
Plain Text | Hoffman, P. F. (1998) A Neoproterozoic Snowball Earth. Science, 281 (5381). 1342-1346 doi:10.1126/science.281.5381.1342 | ||
In | (1998, August) Science Vol. 281 (5381) American Association for the Advancement of Science (AAAS) |
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
M. J. Hambrey and W. B. Harland Earth's Pre-Pleistocene Glacial Record (Cambridge Univ. Press Cambridge 1981). | |
Aitken J. D., Bull. Geol. Surv. Can. 404, 1 (1991); | |
; I. J. Fairchild in Sedimentology Review 1 V. P. Wright Ed. (Blackwell Oxford 1993) pp. 1–16. | |
Although Phanerozoic cool-water skeletal carbonates are not uncommon [N. P. James and J. A. D. Clarke Cool-Water Carbonates (Society for Sedimentary Geology Tulsa OK 1997)] the inverse solubility of CaCO 3 with temperature mitigates against such an origin for inorganic carbonates with abundant aragonitic sea-floor cements which are typical of Neoproterozoic postglacial cap carbonates [ | |
H. Martin The Precambrian Geology of South West Africa and Namaqualand (Precambrian Research Unit University of Cape Town Cape Town South Africa 1965); | |
Kaufman, Alan J, Hayes, J.M, Knoll, Andrew H, Germs, Gerard J.B (1991) Isotopic compositions of carbonates and organic carbon from upper Proterozoic successions in Namibia: stratigraphic variation and the effects of diagenesis and metamorphism. Precambrian Research, 49 (3) 301-327 doi:10.1016/0301-9268(91)90039-d | |
Kaufman A. J., Knoll A. H., ibid. 73, 27 (1995); | |
. The carbon isotopic compositions of carbonates were determined according to procedures described in these references and in (11) and were reported as δ 13 C values relative to Vienna Pee Dee belemnite in units per mil defined as [( R sample / R standard ) − 1] × 10 3 where R = 13 C/ 12 C. | |
Kah L. C., Bartley J. K., Geol. Soc. Am. Abstr. Programs 29, 115 (1997); | |
Sohl L. E., Geol. Soc. Am. Abstr. Programs 29, 195 (1997); | |
P. F. Hoffman A. J. Kaufman G. P. Halverson GSA Today 8 (5) 1 (1998). | |
; Earth Sci. Rev. 34 1 (1993). | |
J. L. Kirschvink [in The Proterozoic Biosphere J. W. Schopf and C. Klein Eds. (Cambridge Univ. Press New York 1992) pp. 51–52] extended an idea originally proposed by W. B. Harland (3). | |
Hoffmann K. H., Prave A. R., Communs. Geol. Surv. Namibia 11, 47 (1996). | |
Discussions of diagenesis in Neoproterozoic carbonates and descriptions of methods for screening samples before isotopic analysis are contained in (10) and (11). | |
Kennedy M. J., Prave A. R., Hoffmann K. H., Geol. Soc. Am. Abstr. Programs 29, 196 (1997). | |
. The time required to achieve meltback would be less if the ice surface became darkened by volcanic ash. However the effect of ash accumulation would be countered by hoarfrost formation that originated from volcanic outgassed H 2 O. Caldeira and Kasting reported the possibility of irreversible icehouse conditions due to the formation of CO 2 clouds as did Kirschvink (17) but it now appears that cooling actually may be limited by CO 2 clouds [ | |
Sea-floor crystal fans pseudomorphic after aragonite (not ikaite) and reeflike in overall construction occur locally in the Maieberg cap carbonate (G. Soffer personal communication). | |
Analysis of tidal rhythmites indicates ∼400 solar days in the late Neoproterozoic year [ | |
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; K. J. Niklas The Evolutionary Biology of Plants (Univ. of Chicago Press Chicago 1997). | |
We thank S. Bowring J. Edmond B. Farrell M. Delaney J. Grotzinger A. Knoll J. Marshall M. McElroy and P. Myrow for discussions. B. Holtzman G. Hu A. Maloof A. Prave G. Soffer and D. Sumner contributed to fieldwork. The manuscript benefited from comments by K. Caldeira L. Derry D. Erwin L. Kump and an anonymous reviewer. This work was supported by NSF grants EAR 95-06769 EAR 95-10339 EAR 96-30928 EAR 96- 14070 and OCE 97-33688; the National Sciences and Engineering Research Council of Canada; the Canadian Institute of Advanced Research; Harvard University; the University of Maryland; and the Geological Survey of Namibia. |
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