Foraminiferal, lithic, and isotopic changes across four major unconformities at Deep Sea Drilling Project Site 548, Goban Spur
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Abstract
Sediment samples taken at close intervals across four major unconformities (middle Miocene/upper Miocene, lower Oligocene/upper Oligocene, lower Eocene/upper Eocene, lower Paleocene/upper Paleocene) at DSDP-IPOD Site 548, Goban Spur, reveal that coeval biostratigraphic gaps, sediment discontinuities, and seismic unconformities coincide with postulated low stands of sea level. Foraminiferal, lithic, and isotopic analyses demonstrate that environments began to shift prior to periods of marine erosion, and that sedimentation resumed in the form of turbidites derived from nearby upper-slope sources. The unconformities appear to have developed where a water-mass boundary intersected the continental slope, rhythmically crossing the drill site in concert with sea-level rise and fall.
Study Area
Publication type | Book chapter |
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Publication Subtype | Book Chapter |
Title | Foraminiferal, lithic, and isotopic changes across four major unconformities at Deep Sea Drilling Project Site 548, Goban Spur |
Chapter | 14 |
DOI | 10.2973/dsdp.proc.80.114.1985 |
Volume | 80 |
Year Published | 1985 |
Language | English |
Publisher | Ocean Drilling Program |
Contributing office(s) | Coastal and Marine Geology Program, Woods Hole Coastal and Marine Science Center |
Description | 17 p. |
Larger Work Type | Book |
Larger Work Subtype | Monograph |
Larger Work Title | Initial reports of the Deep Sea Drilling Project |
First page | 539 |
Last page | 555 |
Country | Ireland |
Other Geospatial | Atlantic Ocean, Goban Spur |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |