rdf-syntax-grammar
mods:
  schema location: http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-2.xsd
  title info:
    title: Deglacial patterns of South Pacific overturning inferred from 231Pa and 230Th
  title info:
    title: Deglacial patterns of South Pacific overturning inferred from 231 Pa and 230 Th
  name:
    name part: Ronge, Thomas
    role:
      role term: creator
    role:
      role term: VerfasserIn
    role:
      role term: aut
  name:
    name part: Lippold, Jörg
    role:
      role term: VerfasserIn
    role:
      role term: aut
  name:
    name part: Geibert, Walter
    role:
      role term: VerfasserIn
    role:
      role term: aut
  name:
    name part: Jaccard, Samuel L.
    role:
      role term: VerfasserIn
    role:
      role term: aut
  name:
    name part: Mieruch-Schnülle, Sebastian
    role:
      role term: VerfasserIn
    role:
      role term: aut
  name:
    name part: Süfke, Finn
    name part: 1988-
    role:
      role term: VerfasserIn
    role:
      role term: aut
  name:
    name part: Tiedemann, Ralf
    role:
      role term: VerfasserIn
    role:
      role term: aut
  type of resource: text
  origin info:
    place:
      place term: xx
    date issued: 2021
    issuance: monographic
  language:
    language term: eng
  physical description:
    form: remote
    extent: 11
  abstract: The millennial-scale variability of the Atlantic Meridional Overturning Circulation (AMOC) is well documented for the last glacial termination and beyond. Despite its importance for the climate system, the evolution of the South Pacific overturning circulation (SPOC) is by far less well understood. A recently published study highlights the potential applicability of the 231Pa/230Th-proxy in the Pacific. Here, we present five sedimentary down-core profiles of 231Pa/230Th-ratios measured on a depth transect from the Pacific sector of the Southern Ocean to test this hypothesis using downcore records. Our data are consistent with an increase in SPOC as early as 20 ka that peaked during Heinrich Stadial 1. The timing indicates that the SPOC did not simply react to AMOC changes via the bipolar seesaw but were triggered via Southern Hemisphere processes.
  note: Thomas A. Ronge, Jörg Lippold, Walter Geibert, Samuel L. Jaccard, Sebastian Mieruch-Schnülle, Finn Süfke & Ralf Tiedemann
  note: Im Text sind "231" und "230 "hochgestellt
  note: Gesehen am 24.12.2021
  subject:
    topic: Biogeochemistry
  subject:
    topic: Palaeoceanography
  subject:
    topic: Palaeoclimate
  classification: 31
  related item:
    title info:
      title: Scientific reports
    name:
      name part: Deglacial patterns of South Pacific overturning inferred from 231Pa and 230Th
    origin info:
      publisher: [London] : Springer Nature, 2011
    physical description:
      extent: Online-Ressource
    identifier: 2045-2322
    identifier: (DE-627)663366712
    identifier: (DE-600)2615211-3
    identifier: (DE-576)346641179
    part:
      text: 11(2021), Artikel-ID 20473, Seite 1-11
  related item:
    name:
      name part: Deglacial patterns of South Pacific overturning inferred from 231Pa and 230Th
    part:
      text: volume:11
    part:
      text: year:2021
    part:
      text: elocationid:20473
    part:
      text: pages:1-11
    part:
      text: extent:11
  identifier: https://doi.org/10.1038/s41598-021-00111-1
  identifier: https://www.nature.com/articles/s41598-021-00111-1
  record info:
    record content source: DE-627
    record creation date: 211224
    record change date: 20250704073711.0
    record identifier: 1783564679
    language of cataloging:
      language term: ger