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Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia

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@article{IJASEIT10479,
   author = {Khoiril Anwar Maryunani and Rubiyanto Kapid and - Djuhaeni and Wahyu Dwijo Santoso and Dasapta Erwin Irawan},
   title = {Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia},
   journal = {International Journal on Advanced Science, Engineering and Information Technology},
   volume = {11},
   number = {3},
   year = {2021},
   pages = {1268--1272},
   keywords = {Rembang zone; North East Java basin; biostratigraphy; foraminifera; paleobathymetry; paleoclimate.},
   abstract = {

We studied benthic faunas and planktonic foraminiferas in seven stratigraphic sections in Rembang Zone to understand the paleoecology of the area. Rembang Zone is an interesting object for further examination especially during Plio-Pleistocene. That time fragment holds a very important information of ecological changes in Java Island. We observed the following sections: upper-part of Ledok fm, calcareous shales/marls of Mundu fm, glouconitic Globigerinid sands of Selorejo fm, and blue-green shales of Tambakromo Member of Lidah fm. We identified N21 sequence in the Late Pliocene, with a sequence boundary (SB-21) which is superimposed with irregular contact between marl of Mundu fm and Globigerinid sands of Selorejo fm. This irregular contact is interpreted as the base of an incised valley, which was generated by a falling sea-level event in Late Pliocene. We spot 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 with Past computer software, we describe the correlation between variation of foraminifera and environmental change and the bathymetry zone. We find paleoclimate changes by the presence of sub-tropical transitional faunas (Globorotalia tosaensis tosaensis) and the increasing of tropical fauna (Globorotalia truncatulinoides) in Plio–Pleistocene sediments. 

},    issn = {2088-5334},    publisher = {INSIGHT - Indonesian Society for Knowledge and Human Development},    url = {http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=10479},    doi = {10.18517/ijaseit.11.3.10479} }

EndNote

%A Maryunani, Khoiril Anwar
%A Kapid, Rubiyanto
%A Djuhaeni, -
%A Santoso, Wahyu Dwijo
%A Irawan, Dasapta Erwin
%D 2021
%T Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia
%B 2021
%9 Rembang zone; North East Java basin; biostratigraphy; foraminifera; paleobathymetry; paleoclimate.
%! Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia
%K Rembang zone; North East Java basin; biostratigraphy; foraminifera; paleobathymetry; paleoclimate.
%X 

We studied benthic faunas and planktonic foraminiferas in seven stratigraphic sections in Rembang Zone to understand the paleoecology of the area. Rembang Zone is an interesting object for further examination especially during Plio-Pleistocene. That time fragment holds a very important information of ecological changes in Java Island. We observed the following sections: upper-part of Ledok fm, calcareous shales/marls of Mundu fm, glouconitic Globigerinid sands of Selorejo fm, and blue-green shales of Tambakromo Member of Lidah fm. We identified N21 sequence in the Late Pliocene, with a sequence boundary (SB-21) which is superimposed with irregular contact between marl of Mundu fm and Globigerinid sands of Selorejo fm. This irregular contact is interpreted as the base of an incised valley, which was generated by a falling sea-level event in Late Pliocene. We spot 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 with Past computer software, we describe the correlation between variation of foraminifera and environmental change and the bathymetry zone. We find paleoclimate changes by the presence of sub-tropical transitional faunas (Globorotalia tosaensis tosaensis) and the increasing of tropical fauna (Globorotalia truncatulinoides) in Plio–Pleistocene sediments. 

%U http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=10479 %R doi:10.18517/ijaseit.11.3.10479 %J International Journal on Advanced Science, Engineering and Information Technology %V 11 %N 3 %@ 2088-5334

IEEE

Khoiril Anwar Maryunani,Rubiyanto Kapid,- Djuhaeni,Wahyu Dwijo Santoso and Dasapta Erwin Irawan,"Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia," International Journal on Advanced Science, Engineering and Information Technology, vol. 11, no. 3, pp. 1268-1272, 2021. [Online]. Available: http://dx.doi.org/10.18517/ijaseit.11.3.10479.

RefMan/ProCite (RIS)

TY  - JOUR
AU  - Maryunani, Khoiril Anwar
AU  - Kapid, Rubiyanto
AU  - Djuhaeni, -
AU  - Santoso, Wahyu Dwijo
AU  - Irawan, Dasapta Erwin
PY  - 2021
TI  - Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia
JF  - International Journal on Advanced Science, Engineering and Information Technology; Vol. 11 (2021) No. 3
Y2  - 2021
SP  - 1268
EP  - 1272
SN  - 2088-5334
PB  - INSIGHT - Indonesian Society for Knowledge and Human Development
KW  - Rembang zone; North East Java basin; biostratigraphy; foraminifera; paleobathymetry; paleoclimate.
N2  - 

We studied benthic faunas and planktonic foraminiferas in seven stratigraphic sections in Rembang Zone to understand the paleoecology of the area. Rembang Zone is an interesting object for further examination especially during Plio-Pleistocene. That time fragment holds a very important information of ecological changes in Java Island. We observed the following sections: upper-part of Ledok fm, calcareous shales/marls of Mundu fm, glouconitic Globigerinid sands of Selorejo fm, and blue-green shales of Tambakromo Member of Lidah fm. We identified N21 sequence in the Late Pliocene, with a sequence boundary (SB-21) which is superimposed with irregular contact between marl of Mundu fm and Globigerinid sands of Selorejo fm. This irregular contact is interpreted as the base of an incised valley, which was generated by a falling sea-level event in Late Pliocene. We spot 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 with Past computer software, we describe the correlation between variation of foraminifera and environmental change and the bathymetry zone. We find paleoclimate changes by the presence of sub-tropical transitional faunas (Globorotalia tosaensis tosaensis) and the increasing of tropical fauna (Globorotalia truncatulinoides) in Plio–Pleistocene sediments. 

UR - http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=10479 DO - 10.18517/ijaseit.11.3.10479

RefWorks

RT Journal Article
ID 10479
A1 Maryunani, Khoiril Anwar
A1 Kapid, Rubiyanto
A1 Djuhaeni, -
A1 Santoso, Wahyu Dwijo
A1 Irawan, Dasapta Erwin
T1 Pliocene to Pleistocene Stratigraphy of Rembang Zone, North East Java Basin, Indonesia
JF International Journal on Advanced Science, Engineering and Information Technology
VO 11
IS 3
YR 2021
SP 1268
OP 1272
SN 2088-5334
PB INSIGHT - Indonesian Society for Knowledge and Human Development
K1 Rembang zone; North East Java basin; biostratigraphy; foraminifera; paleobathymetry; paleoclimate.
AB 

We studied benthic faunas and planktonic foraminiferas in seven stratigraphic sections in Rembang Zone to understand the paleoecology of the area. Rembang Zone is an interesting object for further examination especially during Plio-Pleistocene. That time fragment holds a very important information of ecological changes in Java Island. We observed the following sections: upper-part of Ledok fm, calcareous shales/marls of Mundu fm, glouconitic Globigerinid sands of Selorejo fm, and blue-green shales of Tambakromo Member of Lidah fm. We identified N21 sequence in the Late Pliocene, with a sequence boundary (SB-21) which is superimposed with irregular contact between marl of Mundu fm and Globigerinid sands of Selorejo fm. This irregular contact is interpreted as the base of an incised valley, which was generated by a falling sea-level event in Late Pliocene. We spot 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 with Past computer software, we describe the correlation between variation of foraminifera and environmental change and the bathymetry zone. We find paleoclimate changes by the presence of sub-tropical transitional faunas (Globorotalia tosaensis tosaensis) and the increasing of tropical fauna (Globorotalia truncatulinoides) in Plio–Pleistocene sediments. 

LK http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=10479 DO - 10.18517/ijaseit.11.3.10479