(Table 1) Datum-levels from DSDP Hole 80-548

Analyses of benthic Foraminifera carbon isotope values were made in 172 samples from the Late Pliocene at DSDP Site 548 which is located in the Northeast Atlantic on the continental slope southwest of Ireland (1253 m water depth). The carbon isotope record is quite stable from about 3.4 to 2.5 Ma, a...

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Bibliographic Details
Main Author: Loubere, Paul
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
80-548
Age
comment
maximum/old
Age model
Ageprofile Datum Description
Deep Sea Drilling Project
Depth
bottom/max
sediment/rock
top/min
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg80
North Atlantic/SPUR
North Atlantic
Northeast Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.761043
https://doi.org/10.1594/PANGAEA.761043
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761043
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 80-548
Age
comment
maximum/old
Age model
Ageprofile Datum Description
Deep Sea Drilling Project
Depth
bottom/max
sediment/rock
top/min
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg80
North Atlantic/SPUR
spellingShingle 80-548
Age
comment
maximum/old
Age model
Ageprofile Datum Description
Deep Sea Drilling Project
Depth
bottom/max
sediment/rock
top/min
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg80
North Atlantic/SPUR
Loubere, Paul
(Table 1) Datum-levels from DSDP Hole 80-548
topic_facet 80-548
Age
comment
maximum/old
Age model
Ageprofile Datum Description
Deep Sea Drilling Project
Depth
bottom/max
sediment/rock
top/min
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg80
North Atlantic/SPUR
description Analyses of benthic Foraminifera carbon isotope values were made in 172 samples from the Late Pliocene at DSDP Site 548 which is located in the Northeast Atlantic on the continental slope southwest of Ireland (1253 m water depth). The carbon isotope record is quite stable from about 3.4 to 2.5 Ma, and contrasts with the record at Site 552A in the North Atlantic (2311 m water depth) which is much more variable for this time period. The carbon record at Site 548 is also consistently more negative than that of Site 552A. After 2.5 Ma the benthic carbon isotope record of Uvigerina at Site 548 becomes extremely variable with large negative deviations. These isotopic variations might be associated with paleoceanic circulation changes caused by glaciation between 2.5 and 2 Ma. However, paired analyses of Uvigerina and Cibicidoides species for 38 samples within the glacial interval, yield carbon isotopic records which are quite different from one another. The Uvigerina record contains larger negative deviations than does the Cibicidoides record. Also, the isotopic difference between Uvigerina and Cibicidoides increases during glaciations and in a long term trend from 2.5 to 2.0 Ma. The lack of covariance between the Uvigerina and Cibicidoides carbon isotope records indicates that, after 2.5 Ma at Site 548, biotic factors influenced the benthic isotopic record.
format Dataset
author Loubere, Paul
author_facet Loubere, Paul
author_sort Loubere, Paul
title (Table 1) Datum-levels from DSDP Hole 80-548
title_short (Table 1) Datum-levels from DSDP Hole 80-548
title_full (Table 1) Datum-levels from DSDP Hole 80-548
title_fullStr (Table 1) Datum-levels from DSDP Hole 80-548
title_full_unstemmed (Table 1) Datum-levels from DSDP Hole 80-548
title_sort (table 1) datum-levels from dsdp hole 80-548
publisher PANGAEA
publishDate 1987
url https://doi.pangaea.de/10.1594/PANGAEA.761043
https://doi.org/10.1594/PANGAEA.761043
op_coverage LATITUDE: 48.915800 * LONGITUDE: -12.164000 * DATE/TIME START: 1981-06-10T00:00:00 * DATE/TIME END: 1981-06-10T00:00:00 * MINIMUM DEPTH, sediment/rock: 100.35 m * MAXIMUM DEPTH, sediment/rock: 186.00 m
long_lat ENVELOPE(-12.164000,-12.164000,48.915800,48.915800)
genre North Atlantic
Northeast Atlantic
genre_facet North Atlantic
Northeast Atlantic
op_source Supplement to: Loubere, Paul (1987): Late Pliocene variations in the carbon isotope values of North Atlantic benthic Foraminifera: Biotic control of the isotopic record? Marine Geology, 76, 45-56, https://doi.org/10.1016/0025-3227(87)90016-8
op_relation Backman, Jan (1984): Cenozoic calcareous nannofossil biostratigraphy from the North-Eastern Atlantic Ocean-Deep Sea Drilling Project Leg 81. In: Roberts, DG; Schnittker, D; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 81, 403-428, https://doi.org/10.2973/dsdp.proc.81.105.1984
Backman, Jan; Shackleton, Nicholas J (1983): Quantitative biochronology of Pliocene and early Pleistocene calcareous nannofossils from the Atlantic, Indian and Pacific oceans. Marine Micropaleontology, 8(2), 141-170, https://doi.org/10.1016/0377-8398(83)90009-9
Hays, James D; Saito, T; Opdyke, Neil D; Burckle, Lloyd H (1969): Pliocene-Pleistocene sediments of the equatorial Pacific: their paleomagnetic, biostratigraphic, and climatic record. Geological Society of America Bulletin, 80(8), 1481-1514, https://doi.org/10.1130/0016-7606(1969)80%5B1481:PSOTEP%5D2.0.CO;2
Keigwin, Lloyd D (1987): Pliocene Stable-Isotope Record of Deep Sea Drilling Project Site 606: Sequential Events of 18O Enrichment Beginning at 3.1 Ma. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 911-920, https://doi.org/10.2973/dsdp.proc.94.127.1987
Loubere, Paul (1987): Changes in mid-depth North Atlantic and Mediterranean circulation during the Late Pliocene - Isotopic and sedimentological evidence. Marine Geology, 77(1-2), 15-38, https://doi.org/10.1016/0025-3227(87)90081-8
Mazzei, Roberto; Raffi, Isabella; Rio, Domenico; Hamilton, Norman; Cita, Maria Bianca (1979): Calibration of Late Neogene calcareous planktonic datum planes with the paleomagnetic record of Site 397 abd correlation with Moroccan and Mediterranean sections. In: von Rad, U & Ryan, WBF (eds.), Initial Reports Deep Sea Drilling Project, Washington (U.S. Government Printing Office), 47, 375-389, https://doi.org/10.2973/dsdp.proc.47-1.109.1979
Ness, Gordon; Levi, Shaul; Couch, Richard (1980): Marine magnetic anomaly timescales for the Cenozoic and Late Cretaceous: A précis, critique, and synthesis. Reviews of Geophysics, 18(4), 753-770, https://doi.org/10.1029/RG018i004p00753
Raymo, Maureen E; Ruddiman, William F; Clement, Bradford M (1987): Pliocene-Pleistocene paleoceanography of the North Atlantic at Deep Sea Drilling Project Site 609. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 895-901, https://doi.org/10.2973/dsdp.proc.94.125.1987
https://doi.pangaea.de/10.1594/PANGAEA.761043
https://doi.org/10.1594/PANGAEA.761043
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.761043
https://doi.org/10.1016/0025-3227(87)90016-8
https://doi.org/10.2973/dsdp.proc.81.105.1984
https://doi.org/10.1016/0377-8398(83)90009-9
https://doi.org/10.1130/0016-7606(1969)80%5B1481:PSOTEP%5D2.0.CO;2
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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761043 2023-05-15T17:31:38+02:00 (Table 1) Datum-levels from DSDP Hole 80-548 Loubere, Paul LATITUDE: 48.915800 * LONGITUDE: -12.164000 * DATE/TIME START: 1981-06-10T00:00:00 * DATE/TIME END: 1981-06-10T00:00:00 * MINIMUM DEPTH, sediment/rock: 100.35 m * MAXIMUM DEPTH, sediment/rock: 186.00 m 1987-05-24 text/tab-separated-values, 36 data points https://doi.pangaea.de/10.1594/PANGAEA.761043 https://doi.org/10.1594/PANGAEA.761043 en eng PANGAEA Backman, Jan (1984): Cenozoic calcareous nannofossil biostratigraphy from the North-Eastern Atlantic Ocean-Deep Sea Drilling Project Leg 81. In: Roberts, DG; Schnittker, D; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 81, 403-428, https://doi.org/10.2973/dsdp.proc.81.105.1984 Backman, Jan; Shackleton, Nicholas J (1983): Quantitative biochronology of Pliocene and early Pleistocene calcareous nannofossils from the Atlantic, Indian and Pacific oceans. Marine Micropaleontology, 8(2), 141-170, https://doi.org/10.1016/0377-8398(83)90009-9 Hays, James D; Saito, T; Opdyke, Neil D; Burckle, Lloyd H (1969): Pliocene-Pleistocene sediments of the equatorial Pacific: their paleomagnetic, biostratigraphic, and climatic record. Geological Society of America Bulletin, 80(8), 1481-1514, https://doi.org/10.1130/0016-7606(1969)80%5B1481:PSOTEP%5D2.0.CO;2 Keigwin, Lloyd D (1987): Pliocene Stable-Isotope Record of Deep Sea Drilling Project Site 606: Sequential Events of 18O Enrichment Beginning at 3.1 Ma. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 911-920, https://doi.org/10.2973/dsdp.proc.94.127.1987 Loubere, Paul (1987): Changes in mid-depth North Atlantic and Mediterranean circulation during the Late Pliocene - Isotopic and sedimentological evidence. Marine Geology, 77(1-2), 15-38, https://doi.org/10.1016/0025-3227(87)90081-8 Mazzei, Roberto; Raffi, Isabella; Rio, Domenico; Hamilton, Norman; Cita, Maria Bianca (1979): Calibration of Late Neogene calcareous planktonic datum planes with the paleomagnetic record of Site 397 abd correlation with Moroccan and Mediterranean sections. In: von Rad, U & Ryan, WBF (eds.), Initial Reports Deep Sea Drilling Project, Washington (U.S. Government Printing Office), 47, 375-389, https://doi.org/10.2973/dsdp.proc.47-1.109.1979 Ness, Gordon; Levi, Shaul; Couch, Richard (1980): Marine magnetic anomaly timescales for the Cenozoic and Late Cretaceous: A précis, critique, and synthesis. Reviews of Geophysics, 18(4), 753-770, https://doi.org/10.1029/RG018i004p00753 Raymo, Maureen E; Ruddiman, William F; Clement, Bradford M (1987): Pliocene-Pleistocene paleoceanography of the North Atlantic at Deep Sea Drilling Project Site 609. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 895-901, https://doi.org/10.2973/dsdp.proc.94.125.1987 https://doi.pangaea.de/10.1594/PANGAEA.761043 https://doi.org/10.1594/PANGAEA.761043 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Loubere, Paul (1987): Late Pliocene variations in the carbon isotope values of North Atlantic benthic Foraminifera: Biotic control of the isotopic record? Marine Geology, 76, 45-56, https://doi.org/10.1016/0025-3227(87)90016-8 80-548 Age comment maximum/old Age model Ageprofile Datum Description Deep Sea Drilling Project Depth bottom/max sediment/rock top/min DRILL Drilling/drill rig DSDP Glomar Challenger Leg80 North Atlantic/SPUR Dataset 1987 ftpangaea https://doi.org/10.1594/PANGAEA.761043 https://doi.org/10.1016/0025-3227(87)90016-8 https://doi.org/10.2973/dsdp.proc.81.105.1984 https://doi.org/10.1016/0377-8398(83)90009-9 https://doi.org/10.1130/0016-7606(1969)80%5B1481:PSOTEP%5D2.0.CO;2 htt 2023-01-20T08:52:15Z Analyses of benthic Foraminifera carbon isotope values were made in 172 samples from the Late Pliocene at DSDP Site 548 which is located in the Northeast Atlantic on the continental slope southwest of Ireland (1253 m water depth). The carbon isotope record is quite stable from about 3.4 to 2.5 Ma, and contrasts with the record at Site 552A in the North Atlantic (2311 m water depth) which is much more variable for this time period. The carbon record at Site 548 is also consistently more negative than that of Site 552A. After 2.5 Ma the benthic carbon isotope record of Uvigerina at Site 548 becomes extremely variable with large negative deviations. These isotopic variations might be associated with paleoceanic circulation changes caused by glaciation between 2.5 and 2 Ma. However, paired analyses of Uvigerina and Cibicidoides species for 38 samples within the glacial interval, yield carbon isotopic records which are quite different from one another. The Uvigerina record contains larger negative deviations than does the Cibicidoides record. Also, the isotopic difference between Uvigerina and Cibicidoides increases during glaciations and in a long term trend from 2.5 to 2.0 Ma. The lack of covariance between the Uvigerina and Cibicidoides carbon isotope records indicates that, after 2.5 Ma at Site 548, biotic factors influenced the benthic isotopic record. Dataset North Atlantic Northeast Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-12.164000,-12.164000,48.915800,48.915800)

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