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  • 2020-2024  (11)
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  • 1
    Publication Date: 2023-12-18
    Description: Knowledge of the equatorial thermocline is essential for understanding climate changes in the tropical Pacific. Multispecies planktic foraminiferal analyses provide a way to examine temperature distributions and thus the structure of the thermocline. Although the secular thermocline development has been documented back to the late Miocene, the early to middle Miocene interval has rarely been examined. In addition, relationships with the dynamic Antarctic ice sheets remain unclear. Here we investigate the vertical thermal gradient in the upper water column at Integrated Ocean Drilling Program Site U1337 in the eastern equatorial Pacific (EEP) throughout the early to middle Miocene (23.1 to 11.7 Ma). The gradient increased over the Miocene Climatic Optimum, whereas it decreased during the East Antarctic Ice Sheet Expansion (EAIE). Comparison of the EEP record with its western equatorial Pacific (WEP) counterpart suggests that sea surface temperature was more stable in the WEP than in the EEP. We further estimated equatorial thermocline from two diagonal gradients between the EEP and the WEP: thermocline shoaled from 16.7 to 15.7 Ma and tilt weakened between 16.5 and 13.8 Ma. The onset of the "Monterey Excursion" and the reduced Antarctic ice sheet volume would have affected thermocline depth and tilt, respectively. Thermocline depth was likely much deeper compared to Pliocene‐to‐modern conditions. Furthermore, a 4‐point‐based distribution of isotherms (4DI index) was used as a metric of the evenness or unevenness of the isotherm distributions. The 4DI index considerably reduced at around the EAIE and other Mi‐events, reflecting the evenly distributed isotherms under a more glaciated Antarctica.
    Keywords: 321-U1337A; AGE; Dentoglobigerina venezuelana, δ13C; Dentoglobigerina venezuelana, δ18O; Depth, composite revised, adjusted; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; equatorial Pacific; Exp321; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Miocene; Pacific Equatorial Age Transect II / Juan de Fuca; Paragloborotalia siakensis, δ13C; Paragloborotalia siakensis, δ18O; planktic foraminifera; Sample code/label; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 1016 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-12-14
    Description: Understanding planktic foraminiferal depth habitat along with consistent taxonomic concepts is key to accurate reconstruction of paleoceanographic records. The Oligocene‐Pliocene long‐ranging and widely distributed species Dentoglobigerina venezuelana lived in the mixed layer (shallower) during the early Oligocene, whereas the same species calcified at thermocline or subthermocline depths (deeper) during the late Oligocene and Miocene. The exact timing of the species' depth habitat change and its possible relationships with Oligocene climate dynamics remain unknown. Here we reveal isotopic records of D. venezuelana along with the Paragloborotalia siakensis group (a mixed‐layer dweller) by using sediments at Integrated Ocean Drilling Program Site U1334 in the eastern equatorial Pacific throughout the Oligocene. A two‐step depth habitat change of D. venezuelana is apparent: (1) from upper to lower mixed layer (~27.4 Ma) and (2) from lower mixed layer to thermocline depth (~26.3 Ma). In addition, the planktic foraminiferal faunal assemblage experienced a marked change from dominantly thermocline (deeper) species to abundant mixed‐layer (shallower) species, suggesting that depth habitat shifts of D. venezuelana were clearly related to thermocline deepening in the eastern equatorial Pacific. Comparison of the first isotopic shift (~27.4 Ma) at multiple sites (U1334, U1333, and 1218) revealed a southward depth habitat change of D. venezuelana within ~200 kyr, implying overall thermocline deepening with reduced steepness in the eastern equatorial Pacific. We consider that global warming conditions during the late Oligocene likely caused thermocline deepening with upwelling decrease in the eastern equatorial Pacific, guiding D. venezuelana to adapt to greater depths in the water column.
    Keywords: 320-U1334A; Accumulation rate, planktic foraminifera by number; AGE; calculated from Pälike et al., 2010; Cassigerinella chipolensis; Catapsydrax dissimilis; Catapsydrax martini; Catapsydrax unicavus; Chiloguembelina cubensis; Density, dry bulk; Dentoglobigerina altispira globosa; Dentoglobigerina baroemoenensis; Dentoglobigerina galavisi; Dentoglobigerina globularis; Dentoglobigerina pseudovenezuelana; Dentoglobigerina sellii; Dentoglobigerina spp.; Dentoglobigerina tripartita; Dentoglobigerina venezuelana; Depth, composite revised, adjusted; Depth, composite revised, corrected; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dry mass; DSDP/ODP/IODP sample designation; equatorial Pacific; Exp320; Foraminifera; Foraminifera, benthic; Foraminifera, planktic; Globigerina anguliofficinalis; Globigerina angulisuturalis; Globigerina brazieri; Globigerina ciperoensis; Globigerina praebulloides; Globigerinella obesa; Globigerinella praesiphonifera; Globigerinita glutinata; Globigerinita uvula; Globigerinoides spp.; Globoquadrina euapertura; Globoquadrina praedehiscens; Globorotaloides eovariabilis; Globorotaloides hexagona; Globorotaloides permicrus; Globorotaloides testarugosa; Globoturborotalita ouachitaensis; Globoturborotalita woodi connecta; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Number; Oligocene; Pacific Equatorial Age Transect I; Paragloborotalia kugleri; Paragloborotalia nana; Paragloborotalia opima; Paragloborotalia pseudocontinuosa; Paragloborotalia pseudokugleri; Paragloborotalia siakensis; planktic foraminifera; Protentella spp.; Pseudohastigerina naguewichiensis; Ratio; Sample code/label; Sedimentation rate; Subbotina angiporoides; Subbotina corpulenta; Subbotina eocaena; Subbotina gortanii; Subbotina linaperta; Subbotina spp.; Subbotina utilisindex; Tenuitella clemenciae; Tenuitella gemma; Tenuitella munda; Tenuitella neoclemenciae; Tenuitella praestainforthi; Tenuitella spp.; Tenuitellinata angustiumbilicata; Turborotalia ampliapertura; Turborotalia increbescans; Turborotalita quinqueloba
    Type: Dataset
    Format: text/tab-separated-values, 2160 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-12-14
    Description: Understanding planktic foraminiferal depth habitat along with consistent taxonomic concepts is key to accurate reconstruction of paleoceanographic records. The Oligocene‐Pliocene long‐ranging and widely distributed species Dentoglobigerina venezuelana lived in the mixed layer (shallower) during the early Oligocene, whereas the same species calcified at thermocline or subthermocline depths (deeper) during the late Oligocene and Miocene. The exact timing of the species' depth habitat change and its possible relationships with Oligocene climate dynamics remain unknown. Here we reveal isotopic records of D. venezuelana along with the Paragloborotalia siakensis group (a mixed‐layer dweller) by using sediments at Integrated Ocean Drilling Program Site U1334 in the eastern equatorial Pacific throughout the Oligocene. A two‐step depth habitat change of D. venezuelana is apparent: (1) from upper to lower mixed layer (~27.4 Ma) and (2) from lower mixed layer to thermocline depth (~26.3 Ma). In addition, the planktic foraminiferal faunal assemblage experienced a marked change from dominantly thermocline (deeper) species to abundant mixed‐layer (shallower) species, suggesting that depth habitat shifts of D. venezuelana were clearly related to thermocline deepening in the eastern equatorial Pacific. Comparison of the first isotopic shift (~27.4 Ma) at multiple sites (U1334, U1333, and 1218) revealed a southward depth habitat change of D. venezuelana within ~200 kyr, implying overall thermocline deepening with reduced steepness in the eastern equatorial Pacific. We consider that global warming conditions during the late Oligocene likely caused thermocline deepening with upwelling decrease in the eastern equatorial Pacific, guiding D. venezuelana to adapt to greater depths in the water column.
    Keywords: 320-U1334A; AGE; Depth, composite revised, adjusted; Depth, composite revised, corrected; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; equatorial Pacific; Exp320; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Oligocene; Pacific Equatorial Age Transect I; planktic foraminifera; Sample code/label; Sample comment; Size fraction; Species; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 918 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-06-12
    Keywords: Abundance; Amphizygus brooksei; Assipetra sp.; Axopodorhabdus albianus; Biostratigraphic datum; Biscutum constans; Broinsonia enormis; Broinsonia signata; Calculites sp.; Chiastozygus sp.; Climate change; Corollithion kennedyi; Corollithion signum; Cribrosphaerella ehrenbergii; Cyclagelosphaera sp.; DEPTH, sediment/rock; Discorhabdus ignotus; Eiffellithus turriseiffelii; Eprolithus floralis; Eprolithus moratus; Eprolithus octopetalus; Eprolithus rarus; Gartnerago sp.; Grantarhabdus sp.; Haquis circumradiatus; Helicolithus anceps; Helicolithus sp.; large igneous province; mid-Cretaceous; Nannoconus sp.; Northwestern Pacific; Nutrient supply; OAE2_OMZ; Prediscosphaera columnata; Preservation; Quadrum gartneri; Quadrum intermedium; Quadrum sp.; Radiolithus planus; Repagulum parvidentatum; Retecapsa sp.; Rhagodiscus achlyostaurion; Rhagodiscus angustus; Rhagodiscus asper; Rhagodiscus sp.; ROCK; Rock sample; Rotelapillus crenulatus; Sample ID; Seribiscutum sp.; Staurolithites sp.; Tegumentum sp.; Tranolithus orionatus; Watznaueria barnesiae; Watznaueria sp.; Zeugrhabdotus bicrescenticus; Zeugrhabdotus diplogrammus; Zeugrhabdotus embergeri; Zeugrhabdotus erectus; Zeugrhabdotus noeliae
    Type: Dataset
    Format: text/tab-separated-values, 2654 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-06-12
    Keywords: Climate change; Degree of pyritization; DEPTH, sediment/rock; Iron, acid-soluble; Iron in pyrite; large igneous province; mid-Cretaceous; Northwestern Pacific; Nutrient supply; OAE2_OMZ; ROCK; Rock sample; Sample ID; Sulfur, total
    Type: Dataset
    Format: text/tab-separated-values, 1185 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-06-12
    Keywords: Angiosperm/Gymnosperm index; Calculated according to Nakamura et al., (2010); Climate change; DEPTH, sediment/rock; large igneous province; mid-Cretaceous; Northwestern Pacific; Nutrient supply; OAE2_OMZ; ROCK; Rock sample; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-06-12
    Description: Mid-Cretaceous oceanic anoxic event 2 (OAE2) is one of the largest carbon cycle perturbations during the Cretaceous period and is regarded as the analog of the present-day warming of the Earth due to the abrupt increase in pCO2 and global warming. It has been hypothesized that increased pCO2 from an eruption of large igneous provinces (LIPs) during OAE2 produced global warming and increased nutrient delivery from continents to oceans, causing oxygen depletion in the oceans globally. Although the Pacific Ocean and the Asian continent were the largest ocean and landmass during the mid-Cretaceous, only limited studies have been performed on the OAE2 strata in the sections of the Pacific and Asian continental margin. This dataset provides the results of a multiproxy analysis of the OAE2 strata in northwestern Hokkaido, Japan, consisting of calcareous nannofossil biostratigraphy, carbon isotope and osmium isotope stratigraphy, degree of pyritization (DOP), XRF analysis, clay mineral chemistry and biomarker analysis. Our result identified seven volcanic pulses, five of which may have elevated humidity, weathering intensity, and vegetational change in the eastern margin of Asia. Moreover, oxygen depletion occurred simultaneously in the northwest Pacific. Given that these environmental changes in the eastern margin of Asia were penecontemporaneous with the global carbon burial intervals during Oceanic Anoxic Event 2, the elevated nutrient supply from the Asian continental margin to the Pacific Ocean may have, in part, contributed to the worldwide depletion of oxygen of the ocean during Oceanic Anoxic Event 2.
    Keywords: Climate change; large igneous province; mid-Cretaceous; Northwestern Pacific; Nutrient supply
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-06-12
    Keywords: calculated, 2 sigma; Climate change; Correlation coefficient, isotope ratio error; DEPTH, sediment/rock; Initial Osmium isotope composition; initial Osmium isotope composition, standard error; large igneous province; mid-Cretaceous; Northwestern Pacific; Nutrient supply; OAE2_OMZ; Osmium; Osmium, standard error; Osmium-187/Osmium-188, standard error; Osmium-187/Osmium-188 ratio; Osmium-192; Osmium-192, standard error; Rhenium; Rhenium, standard error; Rhenium-187/Osmium-188, standard error; Rhenium-187/Osmium-188 ratio; ROCK; Rock sample; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 686 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-06-12
    Keywords: Chlorite, intensity; Climate change; DEPTH, sediment/rock; Illite, intensity; Illite-Smectite, intensity; Kaolinite, intensity; large igneous province; mid-Cretaceous; Modified Lanson Index; Northwestern Pacific; Nutrient supply; OAE2_OMZ; ROCK; Rock sample; Sample ID; Smectite, intensity
    Type: Dataset
    Format: text/tab-separated-values, 1874 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-06-12
    Keywords: Climate change; DEPTH, sediment/rock; large igneous province; mid-Cretaceous; Northwestern Pacific; Nutrient supply; OAE2_OMZ; ROCK; Rock sample; Sample ID; δ13C, wood
    Type: Dataset
    Format: text/tab-separated-values, 1279 data points
    Location Call Number Limitation Availability
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