(Table S1) Age determination of ODP Site 202-1240
Interannual-decadal variability in the equatorial Pacific El Niño-Southern Oscillation (ENSO) induces climate changes at global scale, but its potential influence during past global climate change is not yet well constrained. New high-resolution eastern equatorial Pacific proxy records of thermoclin...
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Language: | English |
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PANGAEA
2008
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.832117 https://doi.org/10.1594/PANGAEA.832117 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.832117 |
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record_format |
openpolar |
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Open Polar |
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PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
202-1240 Age 14C AMS comment dated dated standard deviation Age model COMPCORE Composite Core DEPTH sediment/rock Equatorial East Pacific Joides Resolution Laboratory code/label Leg202 Ocean Drilling Program ODP |
spellingShingle |
202-1240 Age 14C AMS comment dated dated standard deviation Age model COMPCORE Composite Core DEPTH sediment/rock Equatorial East Pacific Joides Resolution Laboratory code/label Leg202 Ocean Drilling Program ODP Pena, Leopoldo D Cacho, Isabel Ferretti, Patrizia Hall, Michael A (Table S1) Age determination of ODP Site 202-1240 |
topic_facet |
202-1240 Age 14C AMS comment dated dated standard deviation Age model COMPCORE Composite Core DEPTH sediment/rock Equatorial East Pacific Joides Resolution Laboratory code/label Leg202 Ocean Drilling Program ODP |
description |
Interannual-decadal variability in the equatorial Pacific El Niño-Southern Oscillation (ENSO) induces climate changes at global scale, but its potential influence during past global climate change is not yet well constrained. New high-resolution eastern equatorial Pacific proxy records of thermocline conditions present new evidence of strong orbital control in ENSO-like variability over the last 275,000 years. Recurrent intervals of saltier thermocline waters are associated with the dominance of La Niña-like conditions during glacial terminations, coinciding with periods of low precession and high obliquity. The parallel dominance of d13C-depleted waters supports the advection of Antarctic origin waters toward the tropical thermocline. This "oceanic tunneling" is proposed to have reinforced orbitally induced changes in ENSO-like variability, composing a complex high- and low-latitude feedback during glacial terminations. |
format |
Dataset |
author |
Pena, Leopoldo D Cacho, Isabel Ferretti, Patrizia Hall, Michael A |
author_facet |
Pena, Leopoldo D Cacho, Isabel Ferretti, Patrizia Hall, Michael A |
author_sort |
Pena, Leopoldo D |
title |
(Table S1) Age determination of ODP Site 202-1240 |
title_short |
(Table S1) Age determination of ODP Site 202-1240 |
title_full |
(Table S1) Age determination of ODP Site 202-1240 |
title_fullStr |
(Table S1) Age determination of ODP Site 202-1240 |
title_full_unstemmed |
(Table S1) Age determination of ODP Site 202-1240 |
title_sort |
(table s1) age determination of odp site 202-1240 |
publisher |
PANGAEA |
publishDate |
2008 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.832117 https://doi.org/10.1594/PANGAEA.832117 |
op_coverage |
LATITUDE: 0.021850 * LONGITUDE: -86.462630 * DATE/TIME START: 2002-05-16T00:00:00 * DATE/TIME END: 2002-05-16T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 29.27 m |
long_lat |
ENVELOPE(-86.462630,-86.462630,0.021850,0.021850) |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
Pena, Leopoldo D; Cacho, Isabel; Ferretti, Patrizia; Hall, Michael A (2008): El Niño-Southern Oscillation-like variability during glacial terminations and interlatitudinal teleconnections. Paleoceanography, 23(3), PA3101, https://doi.org/10.1029/2008PA001620 Fairbanks, Richard G; Mortlock, Richard A; Chiu, Tzu-Chien; Cao, L; Kaplan, Alexey; Guilderson, Thomas P; Fairbanks, Todd W; Bloom, Arthur L; Grootes, Pieter Meiert; Nadeau, Marie-Josée (2005): Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paired 230Th/234U/238U and 14C dates on pristine corals. Quaternary Science Reviews, 24(16-17), 1781-1796, https://doi.org/10.1016/j.quascirev.2005.04.007 Fischer, Hubertus; Wahlen, Martin; Smith, Jesse; Mastroianni, Derek; Deck, Bruce (1999): Ice core records of atmospheric CO2 around the last three Glacial Terminations. Science, 283(5408), 1712-1714, https://doi.org/10.1126/science.283.5408.1712 Hughen, Konrad A; Baillie, Mike G L; Bard, Edouard; Beck, J Warren; Bertrand, Chanda J H; Blackwell, Paul G; Buck, Caitlin E; Burr, George S; Cutler, Kirsten B; Damon, Paul E; Edwards, R Lawrence; Fairbanks, Richard G; Friedrich, Michael; Guilderson, Thomas P; Kromer, Bernd; McCormac, F Gerry; Manning, Sturt W; Ramsey, Christopher Bronk; Reimer, Paula J; Reimer, Ron W; Remmele, Sabine; Southon, John R; Stuiver, Minze; Talamo, Sahra; Taylor, Frederick W; van der Plicht, Johannes; Weyhenmeyer, Constanze E (2004): Marine04 marine radiocarbon age calibration, 0-26 cal kyr BP. Radiocarbon, 46(3), 1059-1086, https://doi.org/10.1017/S0033822200033002 Ninkovich, D; Shackleton, Nicholas J (1975): Distribution, stratigraphic position and age of ash layer `L` in Panama Basin Region. Earth and Planetary Science Letters, 27(1), 20-34, https://doi.org/10.1016/0012-821X(75)90156-9 Petit, Jean Robert; Basile, Isabelle; Leruyuet, A; Raynaud, Dominique; Lorius, C; Jouzel, Jean; Stiévenard, Michel; Lipenkov, Vladimir Ya; Barkov, Nartsiss I; Kudryashov, B B; Davis, Matthew D; Saltzman, Eric S; Kotlyakov, Vladimir (1997): Four climate cycles in Vostok ice core. Nature, 387(6631), 359-360, https://doi.org/10.1038/387359a0 Shackleton, Nicholas J; Hall, Michael A; Vincent, Edith (2000): Phase relationships between millennial-scale events 64,000-24,000 years ago. Paleoceanography, 15(6), 565-569, https://doi.org/10.1029/2000PA000513 https://doi.pangaea.de/10.1594/PANGAEA.832117 https://doi.org/10.1594/PANGAEA.832117 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.83211710.1029/2008PA00162010.1016/j.quascirev.2005.04.00710.1126/science.283.5408.171210.1017/S003382220003300210.1016/0012-821X(75)90156-910.1038/387359a010.1029/2000PA000513 |
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1810289023513526272 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.832117 2024-09-15T17:48:05+00:00 (Table S1) Age determination of ODP Site 202-1240 Pena, Leopoldo D Cacho, Isabel Ferretti, Patrizia Hall, Michael A LATITUDE: 0.021850 * LONGITUDE: -86.462630 * DATE/TIME START: 2002-05-16T00:00:00 * DATE/TIME END: 2002-05-16T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 29.27 m 2008 text/tab-separated-values, 109 data points https://doi.pangaea.de/10.1594/PANGAEA.832117 https://doi.org/10.1594/PANGAEA.832117 en eng PANGAEA Pena, Leopoldo D; Cacho, Isabel; Ferretti, Patrizia; Hall, Michael A (2008): El Niño-Southern Oscillation-like variability during glacial terminations and interlatitudinal teleconnections. Paleoceanography, 23(3), PA3101, https://doi.org/10.1029/2008PA001620 Fairbanks, Richard G; Mortlock, Richard A; Chiu, Tzu-Chien; Cao, L; Kaplan, Alexey; Guilderson, Thomas P; Fairbanks, Todd W; Bloom, Arthur L; Grootes, Pieter Meiert; Nadeau, Marie-Josée (2005): Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paired 230Th/234U/238U and 14C dates on pristine corals. Quaternary Science Reviews, 24(16-17), 1781-1796, https://doi.org/10.1016/j.quascirev.2005.04.007 Fischer, Hubertus; Wahlen, Martin; Smith, Jesse; Mastroianni, Derek; Deck, Bruce (1999): Ice core records of atmospheric CO2 around the last three Glacial Terminations. Science, 283(5408), 1712-1714, https://doi.org/10.1126/science.283.5408.1712 Hughen, Konrad A; Baillie, Mike G L; Bard, Edouard; Beck, J Warren; Bertrand, Chanda J H; Blackwell, Paul G; Buck, Caitlin E; Burr, George S; Cutler, Kirsten B; Damon, Paul E; Edwards, R Lawrence; Fairbanks, Richard G; Friedrich, Michael; Guilderson, Thomas P; Kromer, Bernd; McCormac, F Gerry; Manning, Sturt W; Ramsey, Christopher Bronk; Reimer, Paula J; Reimer, Ron W; Remmele, Sabine; Southon, John R; Stuiver, Minze; Talamo, Sahra; Taylor, Frederick W; van der Plicht, Johannes; Weyhenmeyer, Constanze E (2004): Marine04 marine radiocarbon age calibration, 0-26 cal kyr BP. Radiocarbon, 46(3), 1059-1086, https://doi.org/10.1017/S0033822200033002 Ninkovich, D; Shackleton, Nicholas J (1975): Distribution, stratigraphic position and age of ash layer `L` in Panama Basin Region. Earth and Planetary Science Letters, 27(1), 20-34, https://doi.org/10.1016/0012-821X(75)90156-9 Petit, Jean Robert; Basile, Isabelle; Leruyuet, A; Raynaud, Dominique; Lorius, C; Jouzel, Jean; Stiévenard, Michel; Lipenkov, Vladimir Ya; Barkov, Nartsiss I; Kudryashov, B B; Davis, Matthew D; Saltzman, Eric S; Kotlyakov, Vladimir (1997): Four climate cycles in Vostok ice core. Nature, 387(6631), 359-360, https://doi.org/10.1038/387359a0 Shackleton, Nicholas J; Hall, Michael A; Vincent, Edith (2000): Phase relationships between millennial-scale events 64,000-24,000 years ago. Paleoceanography, 15(6), 565-569, https://doi.org/10.1029/2000PA000513 https://doi.pangaea.de/10.1594/PANGAEA.832117 https://doi.org/10.1594/PANGAEA.832117 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess 202-1240 Age 14C AMS comment dated dated standard deviation Age model COMPCORE Composite Core DEPTH sediment/rock Equatorial East Pacific Joides Resolution Laboratory code/label Leg202 Ocean Drilling Program ODP dataset 2008 ftpangaea https://doi.org/10.1594/PANGAEA.83211710.1029/2008PA00162010.1016/j.quascirev.2005.04.00710.1126/science.283.5408.171210.1017/S003382220003300210.1016/0012-821X(75)90156-910.1038/387359a010.1029/2000PA000513 2024-07-24T02:31:32Z Interannual-decadal variability in the equatorial Pacific El Niño-Southern Oscillation (ENSO) induces climate changes at global scale, but its potential influence during past global climate change is not yet well constrained. New high-resolution eastern equatorial Pacific proxy records of thermocline conditions present new evidence of strong orbital control in ENSO-like variability over the last 275,000 years. Recurrent intervals of saltier thermocline waters are associated with the dominance of La Niña-like conditions during glacial terminations, coinciding with periods of low precession and high obliquity. The parallel dominance of d13C-depleted waters supports the advection of Antarctic origin waters toward the tropical thermocline. This "oceanic tunneling" is proposed to have reinforced orbitally induced changes in ENSO-like variability, composing a complex high- and low-latitude feedback during glacial terminations. Dataset Antarc* Antarctic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-86.462630,-86.462630,0.021850,0.021850) |