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  • 1
    Publication Date: 2023-06-27
    Description: The Japan Sea experienced bottom water anoxia at the last glacial maximum (LGM) since it is surrounded by four shallow straits, the sill depths of which are close to, or shallower than, the drop in sea level (~120 m) that occurred then. A distinctive negative d18O excursion of planktonic foraminifera also took place during the LGM. This excursion has been interpreted from foraminiferal data as recording a drop in the paleosalinity of surface waters on the assumption of a constant low sea surface temperatures between 34 and 11 ka. We present here a profile of alkenone-based sea surface temperatures (alkenone-SSTs) over the past 36 kyr. Our results suggest that SSTs during the LGM were much higher than those previously assumed. After considering the factors that might affect estimation of alkenone-SSTs and comparisons of core-top alkenone-SSTs values with values for modern seawater we conclude that the higher alkenone-SSTs during the LGM are reliable and reasonable. These warm SSTs were probably caused by radiative equilibrium associated with the development of stable water stratification in the Japan Sea during the LGM.
    Keywords: Age model; Calculated; Calculated from UK37 (Prahl et al., 1988); Calendar age; Cassidulina japonica, δ18O; DEPTH, sediment/rock; GC; Gravity corer; KH-79-3_L3; L3; Neogloboquadrina pachyderma dextral and/or sinistral, δ18O; Oki Ridge; Sea surface temperature; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Heezen, Bruce C; MacGregor, Ian D; Foreman, H P; Forristall, G; Hekel, H; Jones, E J W; Kaneps, Ansis G; Krasheninnikov, Valery A; Okada, H; Ruef, Michael R (1973): The Post-Jurassic Sedimentary Sequence on the Pacific Plate; a Kinematic Interpretation Of Diachronous Deposits. In: Heezen, B.C.; MacGregor, I.D., Initial Reports of the Deep Sea Drilling Project, 20, Initial Reports of the Deep Sea Drilling Project, 20, U.S. Government Printing Office, XX, 725-738, https://doi.org/10.2973/dsdp.proc.20.133.1973
    Publication Date: 2023-08-28
    Description: The sea floor of the western Pacific is covered by five stratigraphic units: (l)an eastward thinning wedge of late Tertiary silty clay, primarily of volcanic origin, (2) a Cretaceous to Tertiary zeolitic red clay, (3) a Late Cretaceous to Tertiary chalk/chert sequence, (4) a Cretaceous clay, and (5) a basal chalk/chert sequence. The basal chalk was deposited on the young crust at the crest of the mid-oceanic ridge, while the upper chalk was deposited beneath the equator, and the abyssal clays were deposited in abyssal depths in mid latitudes. A kinematic model has been constructed that outlines the deposition of these units on growing crust, which not only was displaced westward away from the accretion center of the mid-oceanic ridge, but northward under the equator. The average northward component of motion for the Pacific plate has been 2 cm per year from 0 to 30 m.y. and 4.4 cm per year from 30 to 100 m.y. The deep-sea deposits of the Pacific are basically and systematically time transgressive. Claims of general synchroneity for either lithostratigraphy or acoustostratigraphy are rejected as inconsistent with both the drilling data and the kinematic model of Pacific pelagic stratigraphy. A few more well sampled holes in the ancient Pacific plate combined with an appropriately refined kinematic model should yield a 'rather detailed history of the Pacific plate since the Jurassic.
    Keywords: 20-195; 20-196; 20-198A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg20; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 128 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Goddard, D A; Thompson, G; Jones, E J W; Okada, H (1987): The chemistry and mineralogy of ferromanganese encrustations on rocks from the Sierra Leone Rise, equatorial Mid-Atlantic Ridge and New England Seamount Chain. Marine Geology, 77(1-2), 87-98, https://doi.org/10.1016/0025-3227(87)90084-3
    Publication Date: 2023-09-29
    Description: Chemical and mineralogical compositions of ferromanganese oxide coatings on rocks dredged from the New England Seamounts, the Sierra Leone Rise and the Mid-Atlantic Ridge near the Equator have been determined in an investigation of regional differences in Atlantic ferromanganese deposits. Most encrustations are clearly of hydrogenous origin, consisting mainly of todorokite and delta MnO2, but several recovered from the equatorial fracture zones may be hydrothermal accumulations. Differences in the chemistry of the water column and in growth rates of the ferromanganese coatings may be important in producing this regional contrast in composition. Fine-scale changes in element abundances within the encrustations indicate that the nature of the substrate has little influence on compositional variations.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 4
    Publication Date: 2023-08-28
    Keywords: AII20; AII42-05; AII60-06; AII85; ATII20-02/03; AT-II-20-11; AT-II-20-14; AT-II-20-16; AT-II-20-23; AT-II-20-34; AT-II-20-9; ATII42-05; AT-II-42-1; AT-II-42-2; ATII60-06; AT-II-60-14; AT-II-60-15; AT-II-60-17; AT-II-60-19; AT-II-60-21; AT-II-60-22; ATII85; AT-II-85-10; AT-II-85-11; AT-II-85-12; AT-II-85-13; AT-II-85-14; AT-II-85-16; AT-II-85-17; AT-II-85-18; AT-II-85-19; AT-II-85-2; AT-II-85-20; AT-II-85-21; AT-II-85-22; AT-II-85-23; AT-II-85-6; AT-II-85-7; AT-II-85-8; AT-II-85-9; Atlantic Ocean; Atlantis II (1963); CH35; CH-35-2; CH-35-4-1; Chain; CN35-04; Deposit type; DEPTH, sediment/rock; Description; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; KN61-01; Knorr; KNR61; KNR-61-14; KNR-61-15; KNR-61-16; KNR-61-17; KNR-61-19; KNR-61-23; KNR-61-24; KNR-61-27; KNR-61-28; KNR-61-29; KNR-61-5; KNR-61-8; KNR-61-9; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Shackleton; Shackleton75/1; Shackleton75/1_1197B; Shackleton75/1_1224; Shackleton75/1_1233; Shackleton75/1_1234; Shackleton75/1_1240; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 394 data points
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  • 5
    Publication Date: 2023-08-28
    Keywords: Annan Seamount, Atlantic Ocean; Atlantic Ocean; Atomic absorption spectrometry (AAS); Calcium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Event label; Insoluble residue; Iron; Latitude of event; Longitude of event; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; Sample ID; Shackleton; Shackleton75/1; Shackleton75/1_1224; Shackleton75/1_1225; Shackleton75/1_1233; Shackleton75/1_1234; Shackleton75/1_1240; Sodium; Substrate type; Thickness; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 139 data points
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  • 6
    Publication Date: 2023-08-28
    Keywords: AII85; ATII85; AT-II-85-11; AT-II-85-16; AT-II-85-17; AT-II-85-18; AT-II-85-2; Atlantic Ocean; Atlantis II (1963); Atomic absorption spectrometry (AAS); Calcium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Event label; Insoluble residue; Iron; KN61-01; Knorr; KNR61; KNR-61-28; Latitude of event; Longitude of event; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; Sample ID; Sodium; Substrate type; Thickness; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 7
    Publication Date: 2023-11-23
    Keywords: AII20; AII42-05; AII60-06; ATII20-02/03; AT-II-20-11; AT-II-20-14; AT-II-20-16; AT-II-20-23; AT-II-20-34; AT-II-20-9; ATII42-05; AT-II-42-1; AT-II-42-2; ATII60-06; AT-II-60-14; AT-II-60-15; AT-II-60-17; AT-II-60-19; AT-II-60-22; Atlantic Ocean; Atlantis II (1963); Atomic absorption spectrometry (AAS); Calcium; CH35; CH-35-2; CH-35-4-1; Chain; CN35-04; Cobalt; Copper; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; Insoluble residue; Iron; Latitude of event; Longitude of event; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; Sample ID; Shackleton; Shackleton75/1; Shackleton75/1_1197B; Sodium; Substrate type; Thickness; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 309 data points
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  • 8
    Publication Date: 2023-11-23
    Keywords: Atlantic Ocean; Atomic absorption spectrometry (AAS); Calcium; Cobalt; Copper; DISTANCE; Distance, maximum; Distance, minimum; Dredge; DRG; Elevation of event; Event label; Iron; Latitude of event; Longitude of event; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; Sample ID; Shackleton; Shackleton75/1; Shackleton75/1_1197B; Shackleton75/1_1224; Shackleton75/1_1233; Sodium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 286 data points
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  • 9
    Publication Date: 2023-11-25
    Description: Coccolithophores are globally important marine calcifying phytoplankton. They contribute to the organic carbon pump through the primary production and the ballast of organic matter, and to the carbonate pump through the production of calcium carbonate. Here we compiled all available scanning electron microscopy (SEM) coccolithophore abundance observations. Taxa were standardized following NannoTax3 to a species level where possible. Subspecies (e.a. C. leptoporus subsp. leptoporus and C. leptoporus subsp. quadriperforatus) were grouped as single species. The database contains 2556 abundance observations from 35 different publications. The data span the period of 1993-2017, with observations from all ocean basins and all seasons, and at depths ranging from the surface to 5000 m. We limited our compilation to SEM observations (or observations which further identified samples with SEM) because SEM provides greater detail of coccolithophore diversity than more commonly used polarized light microscopy. Although this limits the number of observations, this allows for a more in-depth analysis of coccolithophore ecology, such as the ecological significance of the coccolithophore life cycle.
    Keywords: Acanthoica acanthifera; Acanthoica acanthos; Acanthoica biscayensis; Acanthoica maxima; Acanthoica quattrospina; Acanthoica spp.; Algirosphaera cucullata; Algirosphaera robusta; Algirosphaera spp.; Alisphaera capulata; Alisphaera extenta; Alisphaera gaudii; Alisphaera ordinata; Alisphaera pinnigera; Alisphaera quadrilatera; Alisphaera spp.; Alisphaera unicornis; Anthosphaera lafourcadii; Anthosphaera periperforata; Anthosphaera spp.; Balaniger virgulosa; Braarudosphaera bigelowii; Calcidiscus leptoporus; Calcidiscus spp.; Calciopappus caudatus; Calciopappus spp.; Calciosolenia brasiliensis; Calciosoleniaceae spp.; Calciosolenia murrayi; Calciosolenia spp.; Calicasphaera blokii; Calicasphaera concava; Calicasphaera diconstricta; Calyptrolithina multipora; Calyptrosphaera cialdii; Calyptrosphaera dentata; Calyptrosphaera heimdalae; Calyptrosphaera sphaeroidea; Canistrolithus spp.; Canistrolithus valliformis; Ceratolithus cristatus; Ceratolithus spp.; Chrysotila carterae; Chrysotila roscoffensis; Coccoliths, other; Coccolithus pelagicus; Corisphaera gracilis; Corisphaera spp.; Corisphaera tyrrheniensis; Coronosphaera maxima; Coronosphaera mediterranea; Coronosphaera spp.; Cyrtosphaera aculeata; Cyrtosphaera cidaris; Cyrtosphaera spp.; DATE/TIME; DEPTH, water; Discosphaera tubifera; Emiliania huxleyi; Ericiolus sp.; Florisphaera profunda; Flosculosphaera calceolariopsis; Formonsella pyramidosa; Gephyrocapsa ericsonii; Gephyrocapsa muellerae; Gephyrocapsa oceanica; Gephyrocapsa ornata; Gephyrocapsa spp.; Gladiolithus flabellatus; Gliscolithus amitakareniae; Hayaster perplexus; Helicosphaera carteri; Helicosphaera cornifera; Helicosphaera hyalina; Helicosphaera pavimentum; Helicosphaera spp.; Helicosphaera wallichii; Helladosphaera cornifera; Helladosphaera pienaarii; Helladosphaera vavilovii; Heterococcolithophores; Holococcolithophora kastriensis; Holococcolithophore spp.; Homozygosphaera spinosa; Homozygosphaera spp.; Homozygosphaera triarcha; Homozygosphaera vercelli; Hughesius youngii; Hymenomonas lacuna; Hymenomonas roseola; Hymenomonas spp.; Jomonlithus spp.; LATITUDE; LONGITUDE; Michaelsarsia adriaticus; Michaelsarsia elegans; Michaelsarsia spp.; Ochrosphaera neapolitana; Oolithotus antillarum; Oolithotus fragilis; Oolithotus spp.; Ophiaster formosus; Ophiaster hydroideus; Ophiaster minimus; Ophiaster reductus; Ophiaster spp.; Palusphaera sp.; Palusphaera spp.; Palusphaera vandelii; Pappomonas borealis; Pappomonas flabellifera; Pappomonas sp.; Pappomonas spp.; Papposphaera arctica; Papposphaera lepida; Papposphaera sagittifera; Papposphaera sp.; Papposphaera spp.; Papposphaera thomsenii; Picarola margalefii; Placorhombus ziveriae; Polycrater sp.; Polycrater spp.; Pontosphaera discopora; Pontosphaera japonica; Pontosphaera multipora; Pontosphaera spp.; Pontosphaera syracusana; Poricalyptra aurisinae; Poricalyptra isselii; Poricalyptra magnaghii; Poritectolithus maximus; Poritectolithus poritectum; Pseudowigwamma scenozonion; Reference/source; Reticulofenestra parvula; Reticulofenestra sessilis; Reticulofenestra spp.; Rhabdosphaera clavigera; Rhabdosphaera spp.; Rhabdosphaera xiphos; Sample method; Scyphosphaera apsteinii; Scyphosphaera spp.; see sample method; Solisphaera helianthiformis; Solisphaera spp.; Sphaerocalyptra adenensis; Sphaerocalyptra dermitzakii; Sphaerocalyptra quadridentata; Sphaerocalyptra sp.; Sphaerocalyptra spp.; Syracolithus bicorium; Syracolithus quadriperforatus; Syracolithus schilleri; Syracolithus sp.; Syracolithus spp.; Syracosphaera amoena; Syracosphaera ampliora; Syracosphaera anthos; Syracosphaera arethusae; Syracosphaera bannockii; Syracosphaera borealis; Syracosphaera castellata; Syracosphaera corolla; Syracosphaera delicata; Syracosphaera dilatata; Syracosphaera epigrosa; Syracosphaera exigua; Syracosphaera florida; Syracosphaera gaarderae; Syracosphaera halldalii; Syracosphaera hastata; Syracosphaera histrica; Syracosphaera lamina; Syracosphaera leptolepis; Syracosphaera marginiporata; Syracosphaera molischii; Syracosphaera nana; Syracosphaera nodosa; Syracosphaera noroitica; Syracosphaera orbiculus; Syracosphaera ossa; Syracosphaera prolongata; Syracosphaera protrudens; Syracosphaera pulchra; Syracosphaera reniformis; Syracosphaera rotula; Syracosphaera sp.; Syracosphaera spp.; Syracosphaera squamosa; Syracosphaera strigilis; Syracosphaera tumularis; Tergestiella adriatica; Tetralithoides quadrilaminata; Turrilithus latericioides; Turrisphaera spp.; Umbellosphaera irregularis; Umbellosphaera spp.; Umbellosphaera tenuis; Umbilicosphaera anulus; Umbilicosphaera foliosa; Umbilicosphaera hulburtiana; Umbilicosphaera sibogae; Umbilicosphaera spp.; Wigwamma antarctica; Wigwamma spp.; Wigwamma triradiata; Zygosphaera amoena; Zygosphaera marsilii
    Type: Dataset
    Format: text/tab-separated-values, 685008 data points
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 31 (1975), S. 271-285 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The distribution of coccolithophores was studied in the neritic environment along the western margin of the Pacific Ocean: the Inland Sea of Seto, Yellow Sea, East China Sea, South China Sea, Java Sea, Timor Sea, Arafura Sea and Gulf of Carpentaria. The coccolithophore community in the Red Sea was also studied for comparison with the Pacific marginal seas. With minor exceptions, the coccolithophore communities were very similar throughout the neritic areas investigated, but differed completely from the pelagic community in three aspects. Firstly, almost all neritic coccolithophores, regardless of species, suffered various degrees and forms of malformation with relation to the morphology of their coccoliths, while such malformation was rare in the pelagic population. Nitrogen deficiency may cause such malformation. Secondly, the diversity of species in these marginal seas was much lower than in the pelagic environment, although no species was found to be exclusively neritic. Emiliania huxleyi, usually ubiquitous in oceanic areas and in various neritic environments of higher latitudes, was scarce, while Gephyrocapsa oceanica dominated the flora throughout the studied areas. Finally, the horizontal and vertical distributions of the neritic populations were sporadic compared to those of the rather uniform pelagic environments.
    Type of Medium: Electronic Resource
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