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  • Supplementary material - Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Research datakeyboard_double_arrow_right Image 2019 Indonesian Publisher:Zenodo
    Authors: Maryunani, Khoiril Anwar; Kapid, Rubiyanto; Djuhaeni, Djuhaeni; Santoso, Wahyu Dwijo; +1 Authors

    doi: 10.5281/zenodo.3525452 , 10.5281/zenodo.3525453

    Abstract We studied seven stratigraphic sections in Rembang Zone, North East Java Basin, Central Java based on quantitative analyses of benthic faunas and planktonic foraminiferas. The parts consist of upper-part of Ledok Formation, calcareous shales/marls of Mundu Formation, glouconitic Globigerinid sands of Selorejo Formation, and blue-green shales of Tambakromo Member of Lidah Formation. We identified an N21 sequence in the Late Pliocene, with a sequence boundary (SB-21) which superimposed with irregular contact between marl of Mundu Formation and Globigerinid sands of Selorejo Formation. This irregular contact was interpreted as the based of Incised Valley, which was generated by falling sea-level in Late Pliocene. Also, we spotted the changes in biostratigraphy, paleobathymetry, and paleoclimate. There are three Pliocene biostragraphies in this section: Globorotalia margaritae zone (N19); Globorotalia miocenica zone (N20 – N21) and Globorotalia tosaensis tosaensis zone (the top of N21). Using cluster analysis, we described the correlation between variation of foraminifera and environmental change as well as bathymetry zone. Paleoclimate changes were observed by the presence of sub-tropical transition faunas (Globorotalia tosaensis tosaensis) and the increasing of tropical fauna as Globorotalia truncatulinoides in Plio–Pleistocene sediments. Status: under review in IJASEIT Funding: P3MI ITB 2018

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ZENODOarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    ZENODO
    Image . 2019
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    ZENODO
    Image . 2019
    License: CC BY
    Data sources: ZENODO
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ZENODOarrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      ZENODO
      Image . 2019
      License: CC BY
      Data sources: Datacite
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      License: CC BY
      Data sources: ZENODO
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The following results are related to Digital Humanities and Cultural Heritage. Are you interested to view more results? Visit OpenAIRE - Explore.

  • Supplementary material - Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Research datakeyboard_double_arrow_right Image 2019 Indonesian Publisher:Zenodo
    Authors: Maryunani, Khoiril Anwar; Kapid, Rubiyanto; Djuhaeni, Djuhaeni; Santoso, Wahyu Dwijo; +1 Authors

    doi: 10.5281/zenodo.3525452 , 10.5281/zenodo.3525453

    Abstract We studied seven stratigraphic sections in Rembang Zone, North East Java Basin, Central Java based on quantitative analyses of benthic faunas and planktonic foraminiferas. The parts consist of upper-part of Ledok Formation, calcareous shales/marls of Mundu Formation, glouconitic Globigerinid sands of Selorejo Formation, and blue-green shales of Tambakromo Member of Lidah Formation. We identified an N21 sequence in the Late Pliocene, with a sequence boundary (SB-21) which superimposed with irregular contact between marl of Mundu Formation and Globigerinid sands of Selorejo Formation. This irregular contact was interpreted as the based of Incised Valley, which was generated by falling sea-level in Late Pliocene. Also, we spotted the changes in biostratigraphy, paleobathymetry, and paleoclimate. There are three Pliocene biostragraphies in this section: Globorotalia margaritae zone (N19); Globorotalia miocenica zone (N20 – N21) and Globorotalia tosaensis tosaensis zone (the top of N21). Using cluster analysis, we described the correlation between variation of foraminifera and environmental change as well as bathymetry zone. Paleoclimate changes were observed by the presence of sub-tropical transition faunas (Globorotalia tosaensis tosaensis) and the increasing of tropical fauna as Globorotalia truncatulinoides in Plio–Pleistocene sediments. Status: under review in IJASEIT Funding: P3MI ITB 2018

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ZENODOarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    ZENODO
    Image . 2019
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    ZENODO
    Image . 2019
    License: CC BY
    Data sources: ZENODO
    Claim

    This Research product is the result of merged Research products in OpenAIRE.

    You have already added works in your ORCID record related to the merged Research product.
    0
    citations0
    popularityAverage
    influenceAverage
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    BIP!Powered by BIP!
    visibility61
    visibilityviews61
    downloaddownloads32
    Powered by Usage counts
    more_vert
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ZENODOarrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      ZENODO
      Image . 2019
      License: CC BY
      Data sources: Datacite
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      ZENODO
      Image . 2019
      License: CC BY
      Data sources: ZENODO
      Claim

      This Research product is the result of merged Research products in OpenAIRE.

      You have already added works in your ORCID record related to the merged Research product.
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