View Item 
      •   IPB Repository
      • IPBana
      • Published by Others
      • Faculty of Agriculture
      • View Item
      •   IPB Repository
      • IPBana
      • Published by Others
      • Faculty of Agriculture
      • View Item
      JavaScript is disabled for your browser. Some features of this site may not work without it.

      Sediments of the Lower Barito Basin in South Kalimantan : Fossil Pollen Composition

      Thumbnail
      View/Open
      Publikasi_Word (32.5Kb)
      Publikasi_pdf (81.76Kb)
      Date
      2010
      Author
      Basuki, Sumawinata
      Metadata
      Show full item record
      Abstract
      こ の論文は国立情報学研究所の学術雑誌公開支援事業により電子化されました。During the present century, Holocene sediments of the lower Barito basin have been reclaimed for agricultural purposes. On Martapura river sediments, stable agricultural plots have been established which are not affected by severe acid toxicity problems : but on Barito river sediments, many plots have been abandoned because of such problems. To clarify the characteristics of the sediments of the lower Barito basin, boring observations were made along two transects on the Barito and Martapura river sediments. The fossil pollen composition, layering patterns, and the presence of sulfidic materials were used to identify the depositional environments of the sediments. This paper presents details of the succession of depositional environments on the Martapura river sediments and Barito river sediments, and demonstrates that the stable agricultural plots belong to a riverine environment. while the unstable agricultural plots belong to a brackish environment. During the present century, Holocene sediments of the lower Barito basin have been reclaimed for agricultural purposes. On Martapura river sediments, stable agricultural plots have been established which are not affected by severe acid toxicity problems : but on Barito river sediments, many plots have been abandoned because of such problems. To clarify the characteristics of the sediments of the lower Barito basin, boring observations were made along two transects on the Barito and Martapura river sediments. The fossil pollen composition, layering patterns, and the presence of sulfidic materials were used to identify the depositional environments of the sediments. This paper presents details of the succession of depositional environments on the Martapura river sediments and Barito river sediments, and demonstrates that the stable agricultural plots belong to a riverine environment. while the unstable agricultural plots belong to a brackish environment.
      URI
      http://repository.ipb.ac.id/handle/123456789/28822
      Collections
      • Faculty of Agriculture [316]

      Copyright © 2020 Library of IPB University
      All rights reserved
      Contact Us | Send Feedback
      Indonesia DSpace Group 
      IPB University Scientific Repository
      UIN Syarif Hidayatullah Institutional Repository
      Universitas Jember Digital Repository
        

       

      Browse

      All of IPB RepositoryCollectionsBy Issue DateAuthorsTitlesSubjectsThis CollectionBy Issue DateAuthorsTitlesSubjects

      My Account

      Login

      Application

      google store

      Copyright © 2020 Library of IPB University
      All rights reserved
      Contact Us | Send Feedback
      Indonesia DSpace Group 
      IPB University Scientific Repository
      UIN Syarif Hidayatullah Institutional Repository
      Universitas Jember Digital Repository