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  • American Geophysical Union  (938)
  • Annual Reviews  (384)
  • Geological Society of America (GSA)
  • PANGAEA
  • 2020-2023  (55)
  • 1970-1974  (1,247)
  • 1935-1939  (63)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Doyle, Patricia S; Boltovskoy, Esteban; Herb, Rene C; Thierstein, Hans R; Hyndman, Roy D; Horvath, George J; Leidy, Rosanne D; McKelvey, Barrie C; Kempe, D R C; Rodolfo, Kelvin S; Davies, Thomas A; Luyendyk, Bruce P (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVI, 1129 pp, https://doi.org/10.2973/dsdp.proc.26.1974
    Publication Date: 2023-08-28
    Description: DSDP Leg 26, is the fifth cruise of D/V Glomar Challenger in the Indian Ocean, and the first cruise of Phase III of the Deep Sea Drilling Project. The Indian Ocean is the smallest of the three major ocean basins but appears to be geologically the most complex. The sites drilled on Leg 26 were selected to try to elucidate a number of specific problems of both local and broad regional significance, as well as to add to the general knowledge of the area. In particular: a) To locate the oldest sediment in the Indian Ocean and thus possibly the date of the initial breakup of Gondwanaland (Sites 250, 256, 257); b) To determine the effects of the initiation of the Circumpolar Current on southern Indian Ocean sedimentation (Sites 250, 252, 256, 257, 258); c) To determine the history of spreading of the Southwest Branch of the Indian Ocean Ridge and the history of the crust and oceanic sedimentation in that general region (Sites 250, 251, 252).
    Keywords: 26-250A; 26-252; 26-256; 26-257; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//BASIN; Leg26; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 2
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2020. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Reviews of Geophysics 58(3), (2020): e2019RG000672, doi:10.1029/2019RG000672.
    Description: Global sea level provides an important indicator of the state of the warming climate, but changes in regional sea level are most relevant for coastal communities around the world. With improvements to the sea‐level observing system, the knowledge of regional sea‐level change has advanced dramatically in recent years. Satellite measurements coupled with in situ observations have allowed for comprehensive study and improved understanding of the diverse set of drivers that lead to variations in sea level in space and time. Despite the advances, gaps in the understanding of contemporary sea‐level change remain and inhibit the ability to predict how the relevant processes may lead to future change. These gaps arise in part due to the complexity of the linkages between the drivers of sea‐level change. Here we review the individual processes which lead to sea‐level change and then describe how they combine and vary regionally. The intent of the paper is to provide an overview of the current state of understanding of the processes that cause regional sea‐level change and to identify and discuss limitations and uncertainty in our understanding of these processes. Areas where the lack of understanding or gaps in knowledge inhibit the ability to provide the needed information for comprehensive planning efforts are of particular focus. Finally, a goal of this paper is to highlight the role of the expanded sea‐level observation network—particularly as related to satellite observations—in the improved scientific understanding of the contributors to regional sea‐level change.
    Description: The research was carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. The authors acknowledge support from the National Aeronautics and Space Administration under Grants 80NSSC17K0565, 80NSSC170567, 80NSSC17K0566, 80NSSC17K0564, and NNX17AB27G. A. A. acknowledges support under GRACE/GRACEFO Science Team Grant (NNH15ZDA001N‐GRACE). T. W. acknowledges support by the National Aeronautics and Space Administration (NASA) under the New (Early Career) Investigator Program in Earth Science (Grant: 80NSSC18K0743). C. G. P was supported by the J. Lamar Worzel Assistant Scientist Fund and the Penzance Endowed Fund in Support of Assistant Scientists at the Woods Hole Oceanographic Institution.
    Keywords: Sea level ; Satellite observations ; Remote sensing
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 3
  • 4
    Publication Date: 2022-05-27
    Description: Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 126(8), (2021): e2021JC017510, https://doi.org/10.1029/2021JC017510.
    Description: The air-sea exchange of oxygen (O2) is driven by changes in solubility, biological activity, and circulation. The total air-sea exchange of O2 has been shown to be closely related to the air-sea exchange of heat on seasonal timescales, with the ratio of the seasonal flux of O2 to heat varying with latitude, being higher in the extratropics and lower in the subtropics. This O2/heat ratio is both a fundamental biogeochemical property of air-sea exchange and a convenient metric for testing earth system models. Current estimates of the O2/heat flux ratio rely on sparse observations of dissolved O2, leaving it fairly unconstrained. From a model ensemble we show that the ratio of the seasonal amplitude of two atmospheric tracers, atmospheric potential oxygen (APO) and the argon-to-nitrogen ratio (Ar/O2), exhibits a close relationship to the O2/heat ratio of the extratropics (40–70°). The amplitude ratio, A APO/A ArN2, is relatively constant within the extratropics of each hemisphere due to the zonal mixing of the atmosphere. A APO/A ArN2 is not sensitive to atmospheric transport, as most of the observed spatial variability in the seasonal amplitude of δAPO is compensated by similar variations in δ(Ar/N2). From the relationship between O2/heat and A APO/A ArN2 in the model ensemble, we determine that the atmospheric observations suggest hemispherically distinct O2/heat flux ratios of 3.3 ± 0.3 and 4.7 ± 0.8 nmol J-1 between 40 and 70° in the Northern and Southern Hemispheres respectively, providing a useful constraint for O2 and heat air-sea fluxes in earth system models and observation-based data products.
    Description: The recent atmospheric measurements of the Scripps program have been supported via funding from the NSF and the National Oceanographic and Atmospheric Administration (NOAA) under grants 1304270 and OAR-CIPO-2015-2004269. M. Manizza and R. F. Keeling thank NSF for financial support via the OCE-1130976 grant. M. Manizza thanks additional financial support from NSF via the ARRA OCE-0850350 grant. S. C. Doney acknowledges support from NSF PLR-1440435. Keith Rodgers acknowledges support from IBS-R028-D1. Gael Forget and the ECCO group kindly provided the ECCOv4 heat fluxes.
    Description: 2022-01-22
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    Publication Date: 2022-10-26
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Wallace, E. J., Donnelly, J. P., van Hengstum, P. J., Winkler, T. S., McKeon, K., MacDonald, D., d'Entremont, N. E., Sullivan, R. M., Woodruff, J. D., Hawkes, A. D., & Maio, C. 1,050 years of hurricane strikes on long island in the Bahamas. Paleoceanography and Paleoclimatology, 36(3), (2021): e2020PA004156, https://doi.org/10.1029/2020PA004156.
    Description: Sedimentary records of past hurricane activity indicate centennial-scale periods over the past millennium with elevated hurricane activity. The search for the underlying mechanism behind these active hurricane periods is confounded by regional variations in their timing. Here, we present a new high resolution paleohurricane record from The Bahamas with a synthesis of published North Atlantic records over the past millennium. We reconstruct hurricane strikes over the past 1,050 years in sediment cores from a blue hole on Long Island in The Bahamas. Coarse-grained deposits in these cores date to the close passage of seven hurricanes over the historical interval. We find that the intensity and angle of approach of these historical storms plays an important role in inducing storm surge near the site. Our new record indicates four active hurricane periods on Long Island that conflict with published records on neighboring islands (Andros and Abaco Island). We demonstrate these three islands do not sample the same storms despite their proximity, and we compile these reconstructions together to create the first regional compilation of annually resolved paleohurricane records in The Bahamas. Integrating our Bahamian compilation with compiled records from the U.S. coastline indicates basin-wide increased storminess during the Medieval Warm Period. Afterward, the hurricane patterns in our Bahamian compilation match those reconstructed along the U.S. East Coast but not in the northeastern Gulf of Mexico. This disconnect may result from shifts in local environmental conditions in the North Atlantic or shifts in hurricane populations from straight-moving to recurving storms over the past millennium.
    Description: This work was funded by the National Science Foundation Graduate Research Fellowship (to E. J. W.), the Dalio Explore Foundation, and National Science Foundation grant OCE-1356708 (to J. P. D. and P. J. vH.).
    Keywords: Bahamas ; Blue holes ; Carbonates ; Paleohurricanes ; Sediment cores
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    Publication Date: 1974-09-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 7
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    PANGAEA
    In:  Supplement to: Andrews, James E; Callender, Edward; Bowser, Carl J; Mero, John L; Gauthier, Michel; Meylan, Maurice A; Craig, James D; Binder, Kenneth; Volk, Patrick; Chave, Alan D; Bachman, Walter (1974): Ferromanganese deposits of the ocean floor. Cruise Report Mn-74-01, R/V Moana Wave, Honolulu to San Diego, 17 July - 10 August 1974. Hawaii Institute of Geophysics, University of Hawaii, Technical Report, 9, 194 pp, https://download.pangaea.de/reference/86495/attachments/08025001_Indexed.pdf
    Publication Date: 2023-08-28
    Description: Cruise MN-74-01 of the R/V Moana Wave was the first part of the field work of the NSF-IDOE Inter-University Ferromanganese Research Program in 1974. This program was designed to investigate the origin, growth, and distribution of copper/nickel-rich manganese nodules in the Pacific Ocean. The field effort was designed to satisfy sample requirements of the 15 principal investigators, while increasing general knowledge of the copper/nickel-rich nodule deposits of the equatorial Pacific. This report is the first of a series of cruise reports designed to assist sample requests for documented nodules, sediment, and water samples so the laboratory results can be realistically compared and related to the environment of nodule growth.
    Keywords: BC; Box corer; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; FFC; FFGR; Free fall corer; Free-fall grab; Latitude of event; Longitude of event; Mass; Mn-74-01-001-FFG-001; Mn-74-01-001-FFG-002; Mn-74-01-001-FFG-003; Mn-74-01-002-FFG-004; Mn-74-01-002-FFG-005; Mn-74-01-002-FFG-006; Mn-74-01-003-FFG-007; Mn-74-01-003-FFG-009; Mn-74-01-004-FFG-010; Mn-74-01-004-FFG-011; Mn-74-01-004-FFG-012; Mn-74-01-005-B2; Mn-74-01-005-FFG-014; Mn-74-01-005-FFG-015; Mn-74-01-006-C5; Mn-74-01-006-FFC-027; Mn-74-01-006-FFG-016; Mn-74-01-006-FFG-017; Mn-74-01-006-FFG-018; Mn-74-01-006-FFG-019; Mn-74-01-006-FFG-020; Mn-74-01-006-FFG-021; Mn-74-01-006-FFG-022; Mn-74-01-006-FFG-023; Mn-74-01-006-FFG-024; Mn-74-01-006-FFG-025; Mn-74-01-006-FFG-026; Mn-74-01-006-FFG-027; Mn-74-01-007-FFG-028; Mn-74-01-007-FFG-029; Mn-74-01-007-FFG-030; Mn-74-01-008-D1; Mn-74-01-008-FFG-032; Mn-74-01-008-FFG-033; Mn-74-01-009-FFG-034; Mn-74-01-009-FFG-036; Mn-74-01-010-FFG-037; Mn-74-01-010-FFG-038; Mn-74-01-010-FFG-039; Mn-74-01-010-FFG-040; Mn-74-01-010-FFG-042; Mn-74-01-010-FFG-043; Mn-74-01-011-FFG-045; Mn-74-01-011-FFG-046; Mn-74-01-011-FFG-047; Mn-74-01 IODE; Moana Wave; MW7401; MW7401-01G01; MW7401-01G02; MW7401-01G03; MW7401-02G04; MW7401-02G05; MW7401-02G06; MW7401-03G07; MW7401-03G09; MW7401-04G10; MW7401-04G11; MW7401-04G12; MW7401-05B02; MW7401-05G14; MW7401-05G15; MW7401-06C05; MW7401-06C07; MW7401-06G16; MW7401-06G17; MW7401-06G18; MW7401-06G19; MW7401-06G20; MW7401-06G21; MW7401-06G22; MW7401-06G23; MW7401-06G24; MW7401-06G25; MW7401-06G26; MW7401-06G27; MW7401-07G28; MW7401-07G29; MW7401-07G30; MW7401-08D01; MW7401-08G32; MW7401-08G33; MW7401-09G34; MW7401-09G36; MW7401-10G37; MW7401-10G38; MW7401-10G39; MW7401-10G40; MW7401-10G42; MW7401-10G43; MW7401-11G45; MW7401-11G46; MW7401-11G47; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nodules, mass abundance; Number; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Shape; Substrate type; Surface description
    Type: Dataset
    Format: text/tab-separated-values, 845 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Hays, J D; Cook, Harry E III; Jenkins, D Graham; Cook, F M; Fuller, J T; Goll, Robert M; Milow, E Dean; Orr, W N (1972): Site 76. In: Hays, J.D.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 9, U.S. Government Printing Office, IX, 21-41, https://doi.org/10.2973/dsdp.proc.9.102.1972
    Publication Date: 2023-08-28
    Description: Site 76 was selected in order to core a thick sequence of sediments north of the Tuamotu ridge that had been crossed by Glomar Challenger justprior to the termination of Leg 8 in Tahiti. Two holes at this site continuously cored 27 meters of lower Pliocene to Recent phillipsitic clay and calcareous nannofossil ooze interbedded with calcareous turbidites. The drill bit was stopped by a silicified calcareous turbidite of Early Pliocene age.
    Keywords: 9-76; 9-76A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Pacific/PLAIN; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Hays, J D; Cook, Harry E III; Jenkins, D Graham; Cook, F M; Fuller, J T; Goll, Robert M; Milow, E Dean; Orr, W N (1972): Site 79. In: Hays, J.D.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 9, U.S. Government Printing Office, IX, 317-400, https://doi.org/10.2973/dsdp.proc.9.105.1972
    Publication Date: 2023-08-28
    Description: Site 79 is located on the crest of the equatorial Pacific sediment belt (Ewing and others, 1968) and is the westernmost of a series of sites (79, 81, 82 and 83) that follow the crest of this belt eastward to and across the crest of the oceanic ridge, locally known as the East Pacific Rise. The purpose of these sites is two-fold: 1) to study variations in biostratigraphy and sediment type from west to east across the Pacific and 2) to paleontologically date basement and determine the rate of spreading of the Pacific plate since the time of deposition of the oldest sediments at Site 77.
    Keywords: 9-79; 9-79A; Comment; Deep Sea Drilling Project; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/VALLEY; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 10
    Publication Date: 1972-12-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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