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- W2021837990 abstract "Research Article| July 01, 2006 Detection of Late Cretaceous eustatic signatures using quantitative biostratigraphy James S. Crampton; James S. Crampton 1GNS Science, P.O. Box 30-368, Lower Hutt, New Zealand Search for other works by this author on: GSW Google Scholar Poul Schiøler; Poul Schiøler 2The Geological Survey of Denmark and Greenland, Ø. Voldgade 10, DK-1350, Copenhagen K., Denmark Search for other works by this author on: GSW Google Scholar Lucia Roncaglia Lucia Roncaglia 3Danish Oil and Natural Gas A/S, Agern Alle 24-26, DK-2970 Hørsholm, Denmark Search for other works by this author on: GSW Google Scholar GSA Bulletin (2006) 118 (7-8): 975–990. https://doi.org/10.1130/B25826.1 Article history received: 26 Mar 2005 rev-recd: 13 Dec 2005 accepted: 10 Mar 2006 first online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation James S. Crampton, Poul Schiøler, Lucia Roncaglia; Detection of Late Cretaceous eustatic signatures using quantitative biostratigraphy. GSA Bulletin 2006;; 118 (7-8): 975–990. doi: https://doi.org/10.1130/B25826.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract This study tested the potential for high-resolution quantitative biostratigraphic methods to distinguish tectonic from supposedly eustatic sequences. The study employed automated multidimensional graphic correlation using constrained optimization (program CONOP). Our analysis was based on 15 onshore sections in eastern New Zealand spanning the Coniacian to Maastrichtian stages (Upper Cretaceous), and 398 well-constrained lowest- or highest-occurrence records derived from 245 dinoflagellate species. The age of the resulting composite section was calibrated using six dated bioevents; two of these events were tied to geochemical or paleomagnetic datums. Following calibration, the composite section had an average relative temporal resolution of less than 130 k.y. through the study interval, although the succession of events was not dated to this level of precision in an absolute sense. Although the CONOP composite will not resolve unconformities or condensed intervals that occur across all studied sections, such “global” unconformities can be identified using clusters of events that are placed at a single composite level. Fifteen major event clusters were identified, 10 of which coincided closely with sequence boundaries identified in the Northern Hemisphere; the probability of this coincidence arising by chance alone is ∼8%. Although these results must be regarded as provisional, they suggest that high-resolution quantitative stratigraphy can provide a potent tool for the identification and correlation of stratigraphic sequences. Furthermore, our findings add significant support for recent studies that have argued for the presence of Late Cretaceous eustasy. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2021837990 title "Detection of Late Cretaceous eustatic signatures using quantitative biostratigraphy" @default.
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