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Nannoplankton Biostratigraphy from Banggai-Sula Basin, Central Sulawesi

Journal of Tropical Biodiversity and Biotechnology · Vol. 9 No. 1 (2024)

DOI
10.22146/jtbb.85308
ISSN
2540-9581, 2540-9573
Terbit
2024-03-11
Penerbit
Universitas Gadjah Mada
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-sa/4.0

Abstrak

The nannoplankton research was conducted in the MH-2 well, Banggai-Sula Basin, Central Sulawesi. Thirty-four ditch-cutting samples were utilized to observe the Minahaki, Kintom, and Biak Formations. Age determination was carried out using biostratigraphy method and standard procedure for first and last occurrence of nannoplankton biodatum and had an absolute age, widely known as a zone indicator. This study aims to determine the age and nannoplankton biozonation of each geological formation in Banggai-Sula Basin. Based on the biostratigraphic analysis, 39 species from 14 genera with abundance frequencies ranging from rare to abundant were found in the MH-2 well. In this study, new results of the age of Banggai-Sula Basin areMiddle Miocene – Early Middle Pliocene (13,706 – 3,727 Ma), and can identify into six calcareous nannoplankton zones that are more detailed than previous researchers, Discoaster signus zone (NN5), Discoaster exilis zone (NN6-NN7), Discoaster berggrenii zone (NN11), Ceratolithus acustus zone (NN12), Helicosphaera sellii zone (NN13-NN15), and the Discoaster tamalis zone (NN16). Biostratigraphic data also shows new information for the first time, the absence of three zones from zone NN8 to zone NN10. This result indicates an unconformity in the Late Miocene age (10.606–8.20 Ma).

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  • Universitas Gadjah Mada
  • Universitas Islam Negeri Ar-Raniry
  • Pertamina (Indonesia)
  • National University of Malaysia
  • Badan Geologi
  • Mulawarman University
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  • Organisasi berbeda
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Rekan penulisOrganisasiArtikel bersama
Sugeng Sapto SurjonoUniversitas Gadjah Mada4
Muhammad Virgiana AAfiliasi tidak diketahui3
Muhammad I. NovianAfiliasi tidak diketahui3
Nugroho Imam SetiawanAfiliasi tidak diketahui3
Sunjaya E.S.Afiliasi tidak diketahui3
Banti T. TampubolonAfiliasi tidak diketahui3
Donan Satria YudhaUniversitas Gadjah Mada2
Rahmadi HidayatUniversitas Gadjah Mada2
Adesti Audina UlfahUniversitas Gadjah Mada2
Moch. Indra NovianAfiliasi tidak diketahui2
Akmaluddin AkmaluddinAfiliasi tidak diketahui1
Ridwan Muhammad HasanUniversitas Islam Negeri Ar-Raniry1
Asmaunizar AsmaunizarUniversitas Islam Negeri Ar-Raniry1
Che Aziz AliNational University of Malaysia1
Rusyad Adi SuriyantoUniversitas Gadjah Mada1
Muhammad Ageng PrabowoUniversitas Gadjah Mada1
Citayana Fani RefaltaUniversitas Gadjah Mada1
Sukahar Eka Adi SaputraBadan Geologi1
Diana RahmawatiMulawarman University1
Wartono RahardjoAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) https://jurnal.ugm.ac.id/jtbb/oai, pertama di-harvest 9 Nov 2026, terakhir terlihat 9 Nov 2026.
Metadata asli (oai_dc)
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	<dc:title xml:lang="en-US">Nannoplankton Biostratigraphy from Banggai-Sula Basin, Central Sulawesi</dc:title>
	<dc:creator>Nurhidayah, Efrilia Mahdilah</dc:creator>
	<dc:creator>Akmaluddin, Akmaluddin</dc:creator>
	<dc:creator>Barianto, Didit Hadi</dc:creator>
	<dc:creator>Husein, Salahuddin</dc:creator>
	<dc:creator>Saripudin, Asep</dc:creator>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:subject xml:lang="en-US">Biostratigraphy; Banggai-Sula Basin; Miocene; Nannoplankton; Unconformity</dc:subject>
	<dc:description xml:lang="en-US">The nannoplankton research was conducted in the MH-2 well, Banggai-Sula Basin, Central Sulawesi. Thirty-four ditch-cutting samples were utilized to observe the Minahaki, Kintom, and Biak Formations. Age determination was carried out using biostratigraphy method and standard procedure for first and last occurrence of nannoplankton biodatum and had an absolute age, widely known as a zone indicator.  This study aims to determine the age and nannoplankton biozonation of each geological formation in Banggai-Sula Basin. Based on the biostratigraphic analysis, 39 species from 14 genera with abundance frequencies ranging from rare to abundant were found in the MH-2 well. In this study, new results of the age of Banggai-Sula Basin areMiddle Miocene – Early Middle Pliocene (13,706 – 3,727 Ma), and can identify into six calcareous nannoplankton zones that are more detailed than previous researchers, Discoaster signus zone (NN5), Discoaster exilis zone (NN6-NN7), Discoaster berggrenii zone (NN11), Ceratolithus acustus zone (NN12), Helicosphaera sellii zone (NN13-NN15), and the Discoaster tamalis zone (NN16). Biostratigraphic data also shows new information for the first time, the absence of three zones from zone NN8 to zone NN10. This result indicates an unconformity in the Late Miocene age (10.606–8.20 Ma). </dc:description>
	<dc:publisher xml:lang="en-US">Universitas Gadjah Mada</dc:publisher>
	<dc:contributor xml:lang="en-US">SKK MIGAS and JOB Pertamina-Medco E&amp;P Tomori Sulawesi</dc:contributor>
	<dc:date>2024-03-11</dc:date>
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	<dc:identifier>https://journal.ugm.ac.id/jtbb/article/view/85308</dc:identifier>
	<dc:identifier>10.22146/jtbb.85308</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Tropical Biodiversity and Biotechnology; Vol 9, No 1 (2024): March; jtbb85308</dc:source>
	<dc:source>2540-9581</dc:source>
	<dc:source>2540-9573</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journal.ugm.ac.id/jtbb/article/view/85308/38409</dc:relation>
	<dc:relation>https://journal.ugm.ac.id/jtbb/article/downloadSuppFile/85308/27030</dc:relation>
	<dc:relation>https://journal.ugm.ac.id/jtbb/article/downloadSuppFile/85308/27031</dc:relation>
	<dc:relation>https://journal.ugm.ac.id/jtbb/article/downloadSuppFile/85308/27237</dc:relation>
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	<dc:rights xml:lang="en-US">Copyright (c) 2024 Journal of Tropical Biodiversity and Biotechnology</dc:rights>
	<dc:rights xml:lang="en-US">http://creativecommons.org/licenses/by-sa/4.0</dc:rights>
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