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The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia

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@article{IJASEIT7573,
   author = {Rubiyanto Kapid and Wahyu Dwijo Santoso and Ben Ikhsan and Moehammad Ali Jambak and Dasapta Erwin Irawan},
   title = {The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia},
   journal = {International Journal on Advanced Science, Engineering and Information Technology},
   volume = {9},
   number = {2},
   year = {2019},
   pages = {594--600},
   keywords = {Mid Miocene Climatic Optimum (MMCO); nannoplankton; temperature changes; Cibulakan formation.},
   abstract = {

Middle Miocene Climatic Optimum (MMCO) is widely distributed and associated with increasing temperature and CO2 content in the atmosphere. The effects of MMCO are identified in the mid-latitude region, with lack of examples from the low latitude areas. In this study, we aim to determine the effect of MMCO at Cibulakan Formation of Bogor Basin, Indonesia, which is situated in lower latitude. We took 58 samples from the Cibulakan Formation, which is exposed along Cileungsi River, for quantitative nannoplankton (the abundance of Helicosphaera carteri) analysis to mark increasing and decreasing salinity event, as they are sensitive to temperature. Temperature relates to the salinity of the seawater due to evaporation. From our analysis, we identified sea surface temperature change in Early Miocene which was presumably due to small scale Early Miocene glaciation and active tectonic during the period. The warmer temperature took place on Middle Miocene as the effect of a warm and open sea environment during Mid Miocene Climatic Optimum. Afterward, the temperature continued to rise until the late Miocene, as it had been triggered by the increasing global temperature at the Pacific Ocean and widely distributed clean water at North West Java Basin during the depositional period.

},    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=7573},    doi = {10.18517/ijaseit.9.2.7573} }

EndNote

%A Kapid, Rubiyanto
%A Santoso, Wahyu Dwijo
%A Ikhsan, Ben
%A Jambak, Moehammad Ali
%A Irawan, Dasapta Erwin
%D 2019
%T The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia
%B 2019
%9 Mid Miocene Climatic Optimum (MMCO); nannoplankton; temperature changes; Cibulakan formation.
%! The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia
%K Mid Miocene Climatic Optimum (MMCO); nannoplankton; temperature changes; Cibulakan formation.
%X 

Middle Miocene Climatic Optimum (MMCO) is widely distributed and associated with increasing temperature and CO2 content in the atmosphere. The effects of MMCO are identified in the mid-latitude region, with lack of examples from the low latitude areas. In this study, we aim to determine the effect of MMCO at Cibulakan Formation of Bogor Basin, Indonesia, which is situated in lower latitude. We took 58 samples from the Cibulakan Formation, which is exposed along Cileungsi River, for quantitative nannoplankton (the abundance of Helicosphaera carteri) analysis to mark increasing and decreasing salinity event, as they are sensitive to temperature. Temperature relates to the salinity of the seawater due to evaporation. From our analysis, we identified sea surface temperature change in Early Miocene which was presumably due to small scale Early Miocene glaciation and active tectonic during the period. The warmer temperature took place on Middle Miocene as the effect of a warm and open sea environment during Mid Miocene Climatic Optimum. Afterward, the temperature continued to rise until the late Miocene, as it had been triggered by the increasing global temperature at the Pacific Ocean and widely distributed clean water at North West Java Basin during the depositional period.

%U http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=7573 %R doi:10.18517/ijaseit.9.2.7573 %J International Journal on Advanced Science, Engineering and Information Technology %V 9 %N 2 %@ 2088-5334

IEEE

Rubiyanto Kapid,Wahyu Dwijo Santoso,Ben Ikhsan,Moehammad Ali Jambak and Dasapta Erwin Irawan,"The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia," International Journal on Advanced Science, Engineering and Information Technology, vol. 9, no. 2, pp. 594-600, 2019. [Online]. Available: http://dx.doi.org/10.18517/ijaseit.9.2.7573.

RefMan/ProCite (RIS)

TY  - JOUR
AU  - Kapid, Rubiyanto
AU  - Santoso, Wahyu Dwijo
AU  - Ikhsan, Ben
AU  - Jambak, Moehammad Ali
AU  - Irawan, Dasapta Erwin
PY  - 2019
TI  - The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia
JF  - International Journal on Advanced Science, Engineering and Information Technology; Vol. 9 (2019) No. 2
Y2  - 2019
SP  - 594
EP  - 600
SN  - 2088-5334
PB  - INSIGHT - Indonesian Society for Knowledge and Human Development
KW  - Mid Miocene Climatic Optimum (MMCO); nannoplankton; temperature changes; Cibulakan formation.
N2  - 

Middle Miocene Climatic Optimum (MMCO) is widely distributed and associated with increasing temperature and CO2 content in the atmosphere. The effects of MMCO are identified in the mid-latitude region, with lack of examples from the low latitude areas. In this study, we aim to determine the effect of MMCO at Cibulakan Formation of Bogor Basin, Indonesia, which is situated in lower latitude. We took 58 samples from the Cibulakan Formation, which is exposed along Cileungsi River, for quantitative nannoplankton (the abundance of Helicosphaera carteri) analysis to mark increasing and decreasing salinity event, as they are sensitive to temperature. Temperature relates to the salinity of the seawater due to evaporation. From our analysis, we identified sea surface temperature change in Early Miocene which was presumably due to small scale Early Miocene glaciation and active tectonic during the period. The warmer temperature took place on Middle Miocene as the effect of a warm and open sea environment during Mid Miocene Climatic Optimum. Afterward, the temperature continued to rise until the late Miocene, as it had been triggered by the increasing global temperature at the Pacific Ocean and widely distributed clean water at North West Java Basin during the depositional period.

UR - http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=7573 DO - 10.18517/ijaseit.9.2.7573

RefWorks

RT Journal Article
ID 7573
A1 Kapid, Rubiyanto
A1 Santoso, Wahyu Dwijo
A1 Ikhsan, Ben
A1 Jambak, Moehammad Ali
A1 Irawan, Dasapta Erwin
T1 The Mid Miocene Climatic Optimum (MMCO) Indication at Low Latitude Sediment Case Study: The Miocene Cibulakan Formation, Bogor Basin, Indonesia
JF International Journal on Advanced Science, Engineering and Information Technology
VO 9
IS 2
YR 2019
SP 594
OP 600
SN 2088-5334
PB INSIGHT - Indonesian Society for Knowledge and Human Development
K1 Mid Miocene Climatic Optimum (MMCO); nannoplankton; temperature changes; Cibulakan formation.
AB 

Middle Miocene Climatic Optimum (MMCO) is widely distributed and associated with increasing temperature and CO2 content in the atmosphere. The effects of MMCO are identified in the mid-latitude region, with lack of examples from the low latitude areas. In this study, we aim to determine the effect of MMCO at Cibulakan Formation of Bogor Basin, Indonesia, which is situated in lower latitude. We took 58 samples from the Cibulakan Formation, which is exposed along Cileungsi River, for quantitative nannoplankton (the abundance of Helicosphaera carteri) analysis to mark increasing and decreasing salinity event, as they are sensitive to temperature. Temperature relates to the salinity of the seawater due to evaporation. From our analysis, we identified sea surface temperature change in Early Miocene which was presumably due to small scale Early Miocene glaciation and active tectonic during the period. The warmer temperature took place on Middle Miocene as the effect of a warm and open sea environment during Mid Miocene Climatic Optimum. Afterward, the temperature continued to rise until the late Miocene, as it had been triggered by the increasing global temperature at the Pacific Ocean and widely distributed clean water at North West Java Basin during the depositional period.

LK http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=7573 DO - 10.18517/ijaseit.9.2.7573