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  • 11
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    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publication Date: 2023-07-10
    Keywords: 42-379A; 42-380; 42-380A; 42-381; Achnanthes brevipes; Actinocyclus divisus; Actinocyclus ehrenbergii; Actinocyclus normannii; Actinocyclus ochotensis; Actinoptychus undulatus; Amphiprora gigantea; Amphora variabilis; Black Sea; Chaetoceros danicus; Chaetoceros peruvianus; Coscinodiscus hungaricus; Coscinodiscus stockesianus; Cyclotella caspia; Cyclotella corona; Cyclotella kutzingiana; Cyclotella praekutzingiana; Cyclotella proshkinae; Cyclotella servant-vildary; Cyclotella servant-vildary elegans; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Epoch; Event label; Glomar Challenger; Gyrosigma acuminatum; Hemiaulus hauckii; Latitude of event; Leg42; Lithologic unit/sequence; Longitude of event; Melosira bellicosa; Melosira elegans; Melosira hibschii; Melosira papilio; Melosira praegranulata; Melosira praeislandica; Microscopy; Period; Rhaphoneis maeotica; Rhizosolenia alata; Rhizosolenia bezrukovii; Rhizosolenia calcar-avis; Rhizosolenia setigera; Sample code/label; Stephanodiscus astraea; Stephanodiscus carconensis; Stephanodiscus dubius; Stephanodiscus hantzschii; Stephanodiscus marginatus; Stephanodiscus pontica; Stephanodiscus prohantzschii; Surirella striatula; Thalassionema nitzschioides; Thalassiosira maeotica; Thalassiosira makarovae; Thalassiosira oestrupii; Thalassiosira subsalina
    Type: Dataset
    Format: text/tab-separated-values, 1566 data points
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  • 12
    Publication Date: 2023-07-10
    Keywords: Ammotium cassis; Archive of Ocean Data; ARCOD; Astrorhiza sp.; Buccella frigida; Buccella inusitata; Bulimina sp.; Calculated; Cassidulina reniforme; Counting 〉50 µm fraction; Cribrostomoides crassimargo; Cribrostomoides sp.; Cyclammina sp.; Cyclogyra sp.; Dentalina baggi; Eggerella advena; Elevation of event; Elphidiella groenlandica; Elphidium bartletti; Elphidium subarcticum; Esosyrinx curta; Event label; Fissurina marginata; Fissurina marginata-perforata; Fissurina ventricosa; Foraminifera, benthic, number of species; Foraminifera, benthic agglutinated; Globigerina spp.; Gordiospira arctica; Grab; GRAB; Hippocrepina indivisa; Hyperammina elongata; Islandiella islandica; Laptev Sea; Laryngosigma sp.; Latitude of event; Longitude of event; Pateoris hauerinoides; Protelphidium depressulum; Protelphidium orbiculare; Pyrgo sp.; Pyrgo williamsoni; Pyrulina sp.; Quinqueloculina agglutinata; Quinqueloculina seminulum; Quinqueloculina stalkeri; Recurvoides contortus; Reophanus oviculus; Reophax arcticus; Reophax curtus; Reophax scorpiurus; Retroelphidium clavatum; Rhizammina alta; Sample code/label; Sorosphaera sp.; SPASIBA-91; Specimen count; Spiroplectammina biformis; Textularia torquata; Thurammina sp.; Trochammina inflata; Trochammina rotaliformis; Trochammina sp.; Yakov Smirnitskiy; YS-1991-1; YS-1991-2; YS-1991-3; YS-1991-36; YS-1991-37; YS-1991-4GR; YS-1991-6; YS-1991-8
    Type: Dataset
    Format: text/tab-separated-values, 784 data points
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  • 13
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    Unknown
    PANGAEA
    In:  Supplement to: Barash, Max S; Kruglikova, Svetlana B; Mukhina, Valentina V (2000): Stratigraphic features of the sedimentary formationsof the Clarion-Clipperton Province (Eastern Equatorial Pacific). Translated from Okeanologiya, 2000, 40(3), 424-433, Oceanology, 40(3), 396-405
    Publication Date: 2023-07-10
    Description: The area in study is characterized by a regional stratigraphic hiatus from Early Miocene to Quaternary. Deposits from Late Eocene to Early Miocene occur on the bottom surface or under a thin sedimentary cover. Ferromanganese nodules, mostly of Oligocene age, formed on surface layers of Tertiary or Quaternary sediments. A detailed micropaleontological study of a block of dense ancient clay coated with a ferromanganese crust was carried out. Composition of found radiolarian and diatomaceous complexes proved that the crust formed in Quaternary on an eroded surface of Late Oligocene clay. In Quaternary Neogene sediments were eroded and washed away by bottom currents. It is likely that the erosion began 0.9-0.7 Ma at the beginning of the "Glacial Pleistocene". The erosion could be initiated by loosening and resuspension of surface sediments resulting from seismic activity generated by strong earthquakes in the Central America subduction zone. The same vibration maintained residual nodules at the seafloor surface. Thus, for the area in study a common reason and a common Quaternary interval for formation of the following features is supposed: a regional stratigraphic hiatus, formation of residual nodule fields, and position of ancient nodules on the surface of Quaternary sediments.
    Keywords: Acrosphaera murrayana; Anthocyrtidium ophirense; Arachnocorallium calvata; Archive of Ocean Data; ARCOD; Arthophormis barbadensis; Artophormis gracilis; Botryocyrtis scutum; Buccinosphaera invaginata; Carpocanium nigriniae; Cestodiscus pulchellus; Collosphaera cribrosa; Collosphaera orthoconus; Collosphaera tuberosa; Cornutella verrucosa; Coscinodiscus craspedodiscus; Cyclampterium pegetrum; Dendrospyris anthocyrtoides; Dictyoprora mongolfieri; Didymocyrtis prismatica; DM41; DM41-3833-12GR; Dmitry Mendeleev; Dorcadospyris ateuchus; Epoch; Euchitonia sp.; Grab; GRAB; Hymeniastrum euclidis; Larcospira quadrangula; Lithomitra elizabethae; Lophophaena hispida; Lychnocanoma elongata; Microscopy; Ommatartus tetrathalamus; Orosphaeridae; Pacific Ocean; Pseudoeunotia doliolus; Pterocanium praetextum; Pterocorys minythorax; Solenosphaera zanguebarica; Spongaster tetras; Stichocorys seriata; Theocorys spongoconum; Theocorythium trachelium; Theocyrtis annosa; Theocyrtis tuberosa; Triceraspyris triceros
    Type: Dataset
    Format: text/tab-separated-values, 429 data points
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  • 14
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    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: Zhuse, Anastasiya P; Mukhina, Valentina V (1973): The Mesocena elliptica Ehr. zone in the Pleistocene sediments of the Pacific Ocean. Oceanology, 13, 386-394
    Publication Date: 2023-09-15
    Description: The Mesocena elliptica Ehr. zone in deep-sea sediments of the Pacific Ocean is characterized by a short vertical range at the base of the Pleistocene section. Depending on sedimentation rate this zone lies at various depths below the ocean bottom. M. elliptica is unknown in recent oceanic plankton. In fossil state known species indicate that sediments containing them are of Oligocene-Miocene age. New data obtained in early 1960's show that within a short interval, evidently in Early Pleistocene, M. elliptica was abundant in plankton, primarily in tropical regions. Correlation of paleomagnetic data with results of diatom analysis shows that the Mesocena elliptica zone always lies above the Pliocene-Pleistocene boundary, and that maximum contents of M. elliptica coincide with the Jaramillo event (0.85-0.95 million years ago).
    Keywords: ALBAT-62; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Pacific Ocean; Thomas G. Thompson (1964); TT028; TT028-14; TT028-17; TT028-19; TT028-22; TT028-23; TT028-24; V24-58; V24-59; V24-60; V24-62; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-34; VITYAZ3802-GC; VITYAZ4599-GC; Vityaz-48; VITYAZ5071-GC; VITYAZ5082-GC; VITYAZ5098-GC; VITYAZ5100-GC; VITYAZ6277-3-GC; VITYAZ6337-GC; Zone boundary, lower; Zone boundary, upper
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
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  • 15
    facet.materialart.
    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: Zhuse, Anastasiya P; Mukhina, Valentina V (1973): The Mesocena elliptica Ehr. zone in the Pleistocene sediments of the Pacific Ocean. Oceanology, 13, 386-394
    Publication Date: 2023-09-15
    Description: The Mesocena elliptica Ehr. zone in deep-sea sediments of the Pacific Ocean is characterized by a short vertical range at the base of the Pleistocene section. Depending on sedimentation rate this zone lies at various depths below the ocean bottom. M. elliptica is unknown in recent oceanic plankton. In fossil state known species indicate that sediments containing them are of Oligocene-Miocene age. New data obtained in early 1960's show that within a short interval, evidently in Early Pleistocene, M. elliptica was abundant in plankton, primarily in tropical regions. Correlation of paleomagnetic data with results of diatom analysis shows that the Mesocena elliptica zone always lies above the Pliocene-Pleistocene boundary, and that maximum contents of M. elliptica coincide with the Jaramillo event (0.85-0.95 million years ago).
    Keywords: ALBAT-62; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Pacific Ocean; Thomas G. Thompson (1964); TT028; TT028-14; TT028-17; TT028-19; TT028-22; TT028-23; TT028-24; V24-58; V24-59; V24-60; V24-62; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-34; VITYAZ3802-GC; VITYAZ4599-GC; Vityaz-48; VITYAZ5071-GC; VITYAZ5082-GC; VITYAZ5098-GC; VITYAZ5100-GC; VITYAZ6277-3-GC; VITYAZ6337-GC; Zone boundary, lower; Zone boundary, upper
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
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  • 16
    Publication Date: 1976-04-01
    Print ISSN: 0026-2803
    Electronic ISSN: 0026-2803
    Topics: Geosciences
    Published by GeoScienceWorld on behalf of Micropaleontology Project.
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