Stratigraphy of Jaten Formation based on palynology and sedimentology analysis in Dongko Area, Trenggalek, East Java
Jaten Formation is located in the Southern Mountains of the eastern part of Java island. East Java is known as one of the largest provinces in Indonesia for oil and gas production. However, the exploited areas have primarily been in the northern part of East Java. The Southern Mountains region shows...
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description | Jaten Formation is located in the Southern Mountains of the eastern part of Java island. East Java is known as one of the largest provinces in Indonesia for oil and gas production. However, the exploited areas have primarily been in the northern part of East Java. The Southern Mountains region shows several indications of potential oil systems, such as shale outcrops in the Jaten Formation. This research aims to understand the stratigraphic characteristics of the Jaten formation using a palynological and sedimentological analysis approach.
The palynological analysis result determined that the age of the Jaten Formation in the study area is estimated to be the upper part of Early Miocene to Middle Miocene, deposited in a back mangrove to mangrove environment. This determination is based on the first appearance datum of the
Stenochlaena areolaris
in the bottom sample (1) and the first appearance datum of the
Florschuetzia meridionalis
in sample 4. An increased proportion of taxa
Acrostichum aureum
,
Calophyllum type
and
Spinizonocolpites echinatus
characterizes the back mangrove environment. The mangrove environment is characterized by an increased proportion of taxa such as
Florscuetzhia trilobata, Florscuetzhia meridionalis, Florscuetzhia levipoli Rhizophora sp, Exoecaria agallocha
and
Avicennia type
. The increased proportion of
Rhizophora
sp pollen primarily influences the high proportion of mangrove taxa. Mangroves with
Rhizophora
sp as their main component are usually found around river estuaries and in areas with periodic influence from the sea, such as lagoons or bays. Based on the sedimentology and palynological analysis, the formation was deposited in mangrove-backmangrove environment. |
doi_str_mv | 10.1088/1755-1315/1339/1/012006 |
format | Article |
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The palynological analysis result determined that the age of the Jaten Formation in the study area is estimated to be the upper part of Early Miocene to Middle Miocene, deposited in a back mangrove to mangrove environment. This determination is based on the first appearance datum of the
Stenochlaena areolaris
in the bottom sample (1) and the first appearance datum of the
Florschuetzia meridionalis
in sample 4. An increased proportion of taxa
Acrostichum aureum
,
Calophyllum type
and
Spinizonocolpites echinatus
characterizes the back mangrove environment. The mangrove environment is characterized by an increased proportion of taxa such as
Florscuetzhia trilobata, Florscuetzhia meridionalis, Florscuetzhia levipoli Rhizophora sp, Exoecaria agallocha
and
Avicennia type
. The increased proportion of
Rhizophora
sp pollen primarily influences the high proportion of mangrove taxa. Mangroves with
Rhizophora
sp as their main component are usually found around river estuaries and in areas with periodic influence from the sea, such as lagoons or bays. Based on the sedimentology and palynological analysis, the formation was deposited in mangrove-backmangrove environment.</description><identifier>ISSN: 1755-1307</identifier><identifier>EISSN: 1755-1315</identifier><identifier>DOI: 10.1088/1755-1315/1339/1/012006</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Chronology ; Estuaries ; Gas production ; Lagoons ; Mangroves ; Miocene ; Mountains ; Oil and gas production ; Outcrops ; Palynology ; Pollen ; Rhizophora ; Sedimentology ; Shale ; Stratigraphy</subject><ispartof>IOP conference series. Earth and environmental science, 2024-05, Vol.1339 (1), p.12006</ispartof><rights>Published under licence by IOP Publishing Ltd</rights><rights>Published under licence by IOP Publishing Ltd. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://iopscience.iop.org/article/10.1088/1755-1315/1339/1/012006/pdf$$EPDF$$P50$$Giop$$Hfree_for_read</linktopdf><link.rule.ids>314,776,780,27901,27902,38845,38867,53815,53842</link.rule.ids></links><search><creatorcontrib>Istiana</creatorcontrib><creatorcontrib>Rachman, M G</creatorcontrib><creatorcontrib>Ardine, J E</creatorcontrib><creatorcontrib>Mustav, I D</creatorcontrib><creatorcontrib>Alfinna, F D S</creatorcontrib><creatorcontrib>Rohaman, M</creatorcontrib><title>Stratigraphy of Jaten Formation based on palynology and sedimentology analysis in Dongko Area, Trenggalek, East Java</title><title>IOP conference series. Earth and environmental science</title><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><description>Jaten Formation is located in the Southern Mountains of the eastern part of Java island. East Java is known as one of the largest provinces in Indonesia for oil and gas production. However, the exploited areas have primarily been in the northern part of East Java. The Southern Mountains region shows several indications of potential oil systems, such as shale outcrops in the Jaten Formation. This research aims to understand the stratigraphic characteristics of the Jaten formation using a palynological and sedimentological analysis approach.
The palynological analysis result determined that the age of the Jaten Formation in the study area is estimated to be the upper part of Early Miocene to Middle Miocene, deposited in a back mangrove to mangrove environment. This determination is based on the first appearance datum of the
Stenochlaena areolaris
in the bottom sample (1) and the first appearance datum of the
Florschuetzia meridionalis
in sample 4. An increased proportion of taxa
Acrostichum aureum
,
Calophyllum type
and
Spinizonocolpites echinatus
characterizes the back mangrove environment. The mangrove environment is characterized by an increased proportion of taxa such as
Florscuetzhia trilobata, Florscuetzhia meridionalis, Florscuetzhia levipoli Rhizophora sp, Exoecaria agallocha
and
Avicennia type
. The increased proportion of
Rhizophora
sp pollen primarily influences the high proportion of mangrove taxa. Mangroves with
Rhizophora
sp as their main component are usually found around river estuaries and in areas with periodic influence from the sea, such as lagoons or bays. Based on the sedimentology and palynological analysis, the formation was deposited in mangrove-backmangrove environment.</description><subject>Chronology</subject><subject>Estuaries</subject><subject>Gas production</subject><subject>Lagoons</subject><subject>Mangroves</subject><subject>Miocene</subject><subject>Mountains</subject><subject>Oil and gas production</subject><subject>Outcrops</subject><subject>Palynology</subject><subject>Pollen</subject><subject>Rhizophora</subject><subject>Sedimentology</subject><subject>Shale</subject><subject>Stratigraphy</subject><issn>1755-1307</issn><issn>1755-1315</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>O3W</sourceid><sourceid>BENPR</sourceid><recordid>eNqFkF1LwzAYhYMoOKe_wYBXwmqTpkmXyzE7Pxh4sXkd0jap3UdTk07ovzelOhEEc5OX857nJBwArjG6w2g6DXFCaYAJpiEmhIc4RDhCiJ2A0XFzepxRcg4unNt4QxITPgLtqrWyrUorm7cOGg2fZatquDB272VTw0w6VUA_NHLX1WZnyg7KuoBerfaqbr8Vv3WVg1UN701dbg2cWSUncG1VXZZyp7YTmErX-vwPeQnOtNw5dfV1j8HrIl3PH4Ply8PTfLYM8ighLNAk4nHOMkVk5g8vcqYlKRiThGeKx9OCUoozRGNOiY5ZJPMCRzzhSmmUR4qMwc2Q21jzflCuFRtzsP6rThBPxYwj_9AYJIMrt8Y5q7RobLWXthMYib5i0Zcn-iJFX7HAYqjYk2QgK9P8RP9P3f5Bpenqt080hSafhvuMDA</recordid><startdate>20240501</startdate><enddate>20240501</enddate><creator>Istiana</creator><creator>Rachman, M G</creator><creator>Ardine, J E</creator><creator>Mustav, I D</creator><creator>Alfinna, F D S</creator><creator>Rohaman, M</creator><general>IOP Publishing</general><scope>O3W</scope><scope>TSCCA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope></search><sort><creationdate>20240501</creationdate><title>Stratigraphy of Jaten Formation based on palynology and sedimentology analysis in Dongko Area, Trenggalek, East Java</title><author>Istiana ; Rachman, M G ; Ardine, J E ; Mustav, I D ; Alfinna, F D S ; Rohaman, M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2736-f3294c6be3abbbb9dc6fa3d66a39be948d5551b054953f462acd12979eef0c2e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Chronology</topic><topic>Estuaries</topic><topic>Gas production</topic><topic>Lagoons</topic><topic>Mangroves</topic><topic>Miocene</topic><topic>Mountains</topic><topic>Oil and gas production</topic><topic>Outcrops</topic><topic>Palynology</topic><topic>Pollen</topic><topic>Rhizophora</topic><topic>Sedimentology</topic><topic>Shale</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Istiana</creatorcontrib><creatorcontrib>Rachman, M G</creatorcontrib><creatorcontrib>Ardine, J E</creatorcontrib><creatorcontrib>Mustav, I D</creatorcontrib><creatorcontrib>Alfinna, F D S</creatorcontrib><creatorcontrib>Rohaman, M</creatorcontrib><collection>IOP Publishing Free Content</collection><collection>IOPscience (Open Access)</collection><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><jtitle>IOP conference series. Earth and environmental science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Istiana</au><au>Rachman, M G</au><au>Ardine, J E</au><au>Mustav, I D</au><au>Alfinna, F D S</au><au>Rohaman, M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Stratigraphy of Jaten Formation based on palynology and sedimentology analysis in Dongko Area, Trenggalek, East Java</atitle><jtitle>IOP conference series. Earth and environmental science</jtitle><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><date>2024-05-01</date><risdate>2024</risdate><volume>1339</volume><issue>1</issue><spage>12006</spage><pages>12006-</pages><issn>1755-1307</issn><eissn>1755-1315</eissn><abstract>Jaten Formation is located in the Southern Mountains of the eastern part of Java island. East Java is known as one of the largest provinces in Indonesia for oil and gas production. However, the exploited areas have primarily been in the northern part of East Java. The Southern Mountains region shows several indications of potential oil systems, such as shale outcrops in the Jaten Formation. This research aims to understand the stratigraphic characteristics of the Jaten formation using a palynological and sedimentological analysis approach.
The palynological analysis result determined that the age of the Jaten Formation in the study area is estimated to be the upper part of Early Miocene to Middle Miocene, deposited in a back mangrove to mangrove environment. This determination is based on the first appearance datum of the
Stenochlaena areolaris
in the bottom sample (1) and the first appearance datum of the
Florschuetzia meridionalis
in sample 4. An increased proportion of taxa
Acrostichum aureum
,
Calophyllum type
and
Spinizonocolpites echinatus
characterizes the back mangrove environment. The mangrove environment is characterized by an increased proportion of taxa such as
Florscuetzhia trilobata, Florscuetzhia meridionalis, Florscuetzhia levipoli Rhizophora sp, Exoecaria agallocha
and
Avicennia type
. The increased proportion of
Rhizophora
sp pollen primarily influences the high proportion of mangrove taxa. Mangroves with
Rhizophora
sp as their main component are usually found around river estuaries and in areas with periodic influence from the sea, such as lagoons or bays. Based on the sedimentology and palynological analysis, the formation was deposited in mangrove-backmangrove environment.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1755-1315/1339/1/012006</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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source | IOP Publishing Free Content; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; IOPscience extra |
subjects | Chronology Estuaries Gas production Lagoons Mangroves Miocene Mountains Oil and gas production Outcrops Palynology Pollen Rhizophora Sedimentology Shale Stratigraphy |
title | Stratigraphy of Jaten Formation based on palynology and sedimentology analysis in Dongko Area, Trenggalek, East Java |
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