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Science 23 February 1996: Vol. 271. no. 5252, pp. 1092 - 1095 DOI: 10.1126/science.271.5252.1092
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Reports
Drilling and Dating New Jersey Oligocene-Miocene Sequences: Ice
Volume, Global Sea Level, and Exxon Records
Kenneth G. Miller,
(1)
Gregory S. Mountain
,
the Leg 150 Shipboard Party,
Members of the New Jersey
Coastal Plain Drilling Project
Oligocene to middle Miocene sequence boundaries on the New Jersey
coastal plain (Ocean Drilling Project Leg 150X) and continental slope
(Ocean Drilling Project Leg 150) were dated by integrating strontium
isotopic stratigraphy, magnetostratigraphy, and biostratigraphy
(planktonic foraminifera, nannofossils, dinocysts, and diatoms). The
ages of coastal plain unconformities and slope seismic reflectors
(unconformities or stratal breaks with no discernible hiatuses) match
the ages of global 18O increases (inferred
glacioeustatic lowerings) measured in deep-sea sites. These
correlations confirm a causal link between coastal plain and slope
sequence boundaries: both formed during global sea-level lowerings. The
ages of New Jersey sequence boundaries and global 18O
increases also correlate well with the Exxon Production Research
sea-level records of Haq et al. and Vail et al.,
validating and refining their compilations.
K. G. Miller, Department of Geological Sciences, Rutgers
University, Piscataway, NJ 08855, USA, and Lamont-Doherty Earth
Observatory of Columbia University, Palisades, NY 10964, USA.
G. S. Mountain, Lamont-Doherty Earth Observatory of Columbia
University, Palisades, NY 10964, USA.
The members of the Leg 150 shipboard party and the New Jersey Coastal
Plain Drilling Project are listed .
(1) To whom correspondence should be addressed.
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Deep Drilling into the Chesapeake Bay Impact Structure.
- G. S. Gohn, C. Koeberl, K. G. Miller, W. U. Reimold, J. V. Browning, C. S. Cockell, J. W. Horton Jr., T. Kenkmann, A. A. Kulpecz, D. S. Powars, et al. (2008)
Science
320, 1740-1745
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- Eocene Oligocene global climate and sea-level changes: St. Stephens Quarry, Alabama.
- K. G. Miller, J. V. Browning, M.-P. Aubry, B. S. Wade, M. E. Katz, A. A. Kulpecz, and J. D. Wright (2008)
Geological Society of America Bulletin
120, 34-53
| Abstract »
| Full Text »
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- Inferring phenotypic evolution in the fossil record by Bayesian inversion.
- B. Hannisdal (2007)
Paleobiology
33, 98-115
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- Quantification of the effects of eustasy, subsidence, and sediment supply on Miocene sequences, mid-Atlantic margin of the United States.
- J. V. Browning, K. G. Miller, P. P. McLaughlin, M. A. Kominz, P. J. Sugarman, D. Monteverde, M. D. Feigenson, and J. C. Hernandez (2006)
Geological Society of America Bulletin
118, 567-588
| Abstract »
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- Chemostratigraphy in Miocene heterozoan carbonate settings: applications, limitations and perspectives.
- M. Mutti, C. M. John, and A. C. Knoerich (2006)
Geological Society, London, Special Publications
255, 307-322
| Abstract »
| PDF »
- The Miocene New Jersey Passive Margin as a Model for the Distribution of Sedimentary Organic Matter in Siliciclastic Deposits.
- C. Pellaton and G. E. Gorin (2005)
Journal of Sedimentary Research
75, 1011-1027
| Abstract »
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- Glacioeustatic changes in the early and middle Eocene (51-42 Ma): Shallow-water stratigraphy from ODP Leg 189 Site 1171 (South Tasman Rise) and deep-sea {delta}18O records.
- S. F. Pekar, A. Hucks, M. Fuller, and S. Li (2005)
Geological Society of America Bulletin
117, 1081-1093
| Abstract »
| Full Text »
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- Relative Control of Paleoceanography, Climate, and Eustasy over Heterozoan Carbonates: A Perspective from Slope Sediments of the Marion Plateau (ODP LEG 194).
- C. M. John and M. Mutti (2005)
Journal of Sedimentary Research
75, 216-230
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- Controls on sequence stratigraphy of a middle Miocene-Holocene, current-swept, passive margin: Offshore Canterbury Basin, New Zealand.
- H. Lu and C. S. Fulthorpe (2004)
Geological Society of America Bulletin
116, 1345-1366
| Abstract »
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- Mixed carbonate-siliciclastic record on the North African margin (Malta)--coupling of weathering processes and mid Miocene climate.
- C. M. John, M. Mutti, and T. Adatte (2003)
Geological Society of America Bulletin
115, 217-229
| Abstract »
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- A New Geochemical-Sequence Stratigraphic Model for the Mahakam Delta and Makassar Slope, Kalimantan, Indonesia: Reply.
- (2001)
AAPG Bulletin
85, 1102-1105
- Oligocene eustasy from two-dimensional sequence stratigraphic backstripping.
- M. A. Kominz and S. F. Pekar (2001)
Geological Society of America Bulletin
113, 291-304
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- Morphology and distribution of Miocene slope incisions off New Jersey: Are they diagnostic of sequence boundaries?.
- C. S. Fulthorpe, J. A. Austin Jr., and G. S. Mountain (2000)
Geological Society of America Bulletin
112, 817-828
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