Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ...
During ODP Leg 166, the recovery of cores from a transect of drill sites across the Bahamas margin from marginal to deep basin environments was an essential requirement for the study of the response of the sedimentary systems to sea-level changes. A detailed biostratigraphy based on planktonic foram...
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ftdatacite:10.1594/pangaea.742696 2023-05-15T18:00:55+02:00 Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... Spezzaferri, Silvia McKenzie, Judith A Isern, Alexandra R 2002 application/zip https://dx.doi.org/10.1594/pangaea.742696 https://doi.pangaea.de/10.1594/PANGAEA.742696 en eng PANGAEA https://dx.doi.org/10.1016/s0025-3227(01)00292-4 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg166 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2002 ftdatacite https://doi.org/10.1594/pangaea.74269610.1016/s0025-3227(01)00292-4 2023-04-03T13:12:12Z During ODP Leg 166, the recovery of cores from a transect of drill sites across the Bahamas margin from marginal to deep basin environments was an essential requirement for the study of the response of the sedimentary systems to sea-level changes. A detailed biostratigraphy based on planktonic foraminifera was performed on ODP Hole 1006A for an accurate stratigraphic control. The investigated late middle Miocene-early Pliocene sequence spans the interval from about 12.5 Ma (Biozone N12) to approximately 4.5 Ma (Biozone N19). Several bioevents calibrated with the time scale of Berggren et al. (1995a,b) were identified. The ODP Site 1006 benthic oxygen isotope stratigraphy can be correlated to the corresponding deep-water benthic oxygen isotope curve from ODP Site 846 in the Eastern Equatorial Pacific (Shackleton et al., 1995. Proc. ODP Sci. Res. 138, 337-356), which was orbitally tuned for the entire Pliocene into the latest Miocene at 6.0 Ma. The approximate stratigraphic match of the isotopic signals from ... : Supplement to: Spezzaferri, Silvia; McKenzie, Judith A; Isern, Alexandra R (2002): Linking the oxygen isotope record of late Neogene eustasy to sequence stratigraphic patterns along the Bahamas margin: results from a paleoceanographic study of ODP Leg 166, Site 1006 sediments. Marine Geology, 185(1-2), 95-120 ... Article in Journal/Newspaper Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Pacific Shackleton Silvia ENVELOPE(-57.900,-57.900,-63.300,-63.300) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg166 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg166 Joides Resolution Ocean Drilling Program ODP Spezzaferri, Silvia McKenzie, Judith A Isern, Alexandra R Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... |
topic_facet |
Drilling/drill rig Leg166 Joides Resolution Ocean Drilling Program ODP |
description |
During ODP Leg 166, the recovery of cores from a transect of drill sites across the Bahamas margin from marginal to deep basin environments was an essential requirement for the study of the response of the sedimentary systems to sea-level changes. A detailed biostratigraphy based on planktonic foraminifera was performed on ODP Hole 1006A for an accurate stratigraphic control. The investigated late middle Miocene-early Pliocene sequence spans the interval from about 12.5 Ma (Biozone N12) to approximately 4.5 Ma (Biozone N19). Several bioevents calibrated with the time scale of Berggren et al. (1995a,b) were identified. The ODP Site 1006 benthic oxygen isotope stratigraphy can be correlated to the corresponding deep-water benthic oxygen isotope curve from ODP Site 846 in the Eastern Equatorial Pacific (Shackleton et al., 1995. Proc. ODP Sci. Res. 138, 337-356), which was orbitally tuned for the entire Pliocene into the latest Miocene at 6.0 Ma. The approximate stratigraphic match of the isotopic signals from ... : Supplement to: Spezzaferri, Silvia; McKenzie, Judith A; Isern, Alexandra R (2002): Linking the oxygen isotope record of late Neogene eustasy to sequence stratigraphic patterns along the Bahamas margin: results from a paleoceanographic study of ODP Leg 166, Site 1006 sediments. Marine Geology, 185(1-2), 95-120 ... |
format |
Article in Journal/Newspaper |
author |
Spezzaferri, Silvia McKenzie, Judith A Isern, Alexandra R |
author_facet |
Spezzaferri, Silvia McKenzie, Judith A Isern, Alexandra R |
author_sort |
Spezzaferri, Silvia |
title |
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... |
title_short |
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... |
title_full |
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... |
title_fullStr |
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... |
title_full_unstemmed |
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A ... |
title_sort |
stable isotope, seismic sequence boundaries and bioevents in odp hole 166-1006a ... |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://dx.doi.org/10.1594/pangaea.742696 https://doi.pangaea.de/10.1594/PANGAEA.742696 |
long_lat |
ENVELOPE(-57.900,-57.900,-63.300,-63.300) |
geographic |
Pacific Shackleton Silvia |
geographic_facet |
Pacific Shackleton Silvia |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1016/s0025-3227(01)00292-4 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.74269610.1016/s0025-3227(01)00292-4 |
_version_ |
1766170209836597248 |