{"data":{"id":"10.1594/pangaea.728761","type":"dois","attributes":{"doi":"10.1594/pangaea.728761","prefix":"10.1594","suffix":"pangaea.728761","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Berggren, William A","givenName":"William A","familyName":"Berggren","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Neogene planktonic foraminifera from the southern Kerguelen Plateau"}],"publisher":"PANGAEA","container":{},"publicationYear":1992,"subjects":[{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"Leg120","subjectScheme":"Campaign"},{"subject":"Joides Resolution","subjectScheme":"Basis"},{"subject":"Ocean Drilling Program (ODP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1992","dateType":"Issued"}],"language":"en","types":{"ris":"GEN","bibtex":"misc","citeproc":"article","schemaOrg":"Collection","resourceType":"Supplementary Publication Series of Datasets","resourceTypeGeneral":"Collection"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.2973/odp.proc.sr.120.153.1992","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["9 datasets"],"formats":["application/zip"],"version":null,"rightsList":[{"rights":"Creative Commons Attribution 3.0 Unported","rightsUri":"https://creativecommons.org/licenses/by/3.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-3.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"With the exception of a brief (2 m.y.) late Miocene-early Pliocene hiatus, an essentially complete Neogene record was recovered on the Kerguelen Plateau in a calcareous biofacies. The stratigraphic distribution of about 30 taxa of Neogene planktonic foraminifers recovered at Sites 747, 748,and 751 (Central and Southern Kerguelen plateaus; approximately 54°-58°S) is recorded. Faunas are characterized by low diversity and high dominance and exhibit a gradual decline in species numbers (reflecting a concomitant increase in biosiliceous forms, particularly diatoms) from about 10 in the early Miocene to 5-8 in the middle Miocene, 3-4 in the late Miocene, to essentially a lone (Neogloboquadrina pachyderma) form in the Pliocene-Pleistocene. A provisional sevenfold biostratigraphic zonation has been formulated that, together with the recovery of a representative Neogene magnetostratigraphic record, may ultimately lead to a correlation with low-latitude magnetobiostratigraphies. The initial appearance of Neogloboquadrina pachyderma is associated with magnetic polarity Chron (MPC) 4 (~7 Ma) and MPC 4A (\u0026gt;8 Ma) at Sites 747 and 751, respectively.","descriptionType":"Abstract"},{"description":"Supplement to: Berggren, William A (1992): Neogene planktonic foraminifer magnetostratigraphy of the southern Kerguelen Plateau (Sites 747, 748, 751). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 631-647","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"79.8148","northBoundLatitude":"-54.811","southBoundLatitude":"-58.441","westBoundLongitude":"76.794"}},{"geoLocationPlace":"South Indian Ridge, South Indian 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