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Late Miocene Molluscan Stage of Jawa Insight from New Field Studies
Aswana, Sufiati E.b, Kistiani D.b, Yudi Abdurrahman I.b, Dwijo Santoso W.a, Rudyawan A.a, Zin Oo T.c
a Geology Department, Faculty of Earth Sciences and Technology, Institute of Technology Bandung, Bandung, Indonesia
b Geological Museum Bandung, Bandung, Indonesia
c Geology Department, East Yangon University, Yangon Division, Thanlyin Township, Myanmar
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]© Published under licence by IOP Publishing Ltd.Neogene stratigraphic stages of Jawa based on molluscan index fossils firstly compiled by Oostingh in 1938. This concept is widely used by palaeontologists, both for application in and outside Jawa. Based on the estimated ages of previous researchers the Neogene stages from old to young are: Rembangian stage considered equivalent to Early Miocene, Preangerian stage (Middle Miocene), Odengian stage (Upper Miocene), Cheribonian stage (Early Pliocene), Sondian stage (Late Pliocene) and Bantamian stage (Early Pleistocene). Further studies to determine a more precise age of each stage are often difficult due to lack of planktonic foraminifera fossils and other age index fossils within the sedimentary deposits that are mostly shallow marine sediments. This study focuses to re-examine the age of sediments of Preangerian and Odengian Stages on new field studies. The type locality and rock units that are correlated with these stages are part of the well-exposed Nyalindung formation around Sukabumi area. The studies were carried out in four main fosill-rich sedimentary sequences that are exposed along Cijarian, Citalahab, Ciangsana and Ciodeng rivers. More detailed ages were obtained from the sediments. The exposed sequences along the Ciangsana and Citalahab rivers are Middle Miocene (N9-N14) while the Cijarian and Ciodeng rivers sequences were deposited between Middle to early Late Miocene (N9-N16). The Nyalindung formation in the Cijarian river also contain Vicarya sp, an index fossil that marks a rise in sea level in the Miocene (12 Ma), which previously only been reported from the Ciangsana river sediments.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Early pleistocene,Jawa,Late Miocene,Molluscan,Neo genes,Planktonic foraminifera,Sedimentary deposits,Sedimentary sequence[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Age,Jawa,Late Miocene,Molluscan,Neogene[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1088/1755-1315/71/1/012031[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]