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  • 1
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    Online Resource
    SITUS LAMBANAPU: DIASPORA AUSTRONESIA DI SUMBA TIMUR
    National Research and Innovation Agency ; 2018
    In:  AMERTA Vol. 36, No. 2 ( 2018-12-16), p. 67-
    Details
    In: AMERTA, National Research and Innovation Agency, Vol. 36, No. 2 ( 2018-12-16), p. 67-
    Abstract: Abstract, Lambanapu Site: Diaspora Austronesia In East Sumba. The research at Lambanapu Site aims to determine the position of Lambanapu in the distribution and development of Austronesian ancestors and their culture in Sumba. The method used is survey, excavation, analysis, and interpretation. The results of the research are skeletal findings and urn burial also artifacts which are pottery, beads, metal jewelry, and stone tools.  From the dating result it is known that Lambanapu Site was inhabited at least 2.000 years ago and from paleantropology analysis, it is estimated that the individuals found from primary and secondary burial in Lambanapu are a mixture of Mongoloid and Australomelanesoid. Genetic mixing is very possible, given the history of the archipelago's occupation which was filled by several waves of great migration in the past. The Lambanapu site has provided an overview of Sumba's ancestral life in the context of the archipelago. The Lamabanapu research results show us, how Lambanapu and Sumba in general rich with historical and cultural values of the past that are very useful for today's life. The wealth of historical and cultural values is not only for local interests, but also to fill the rich history and culture of the archipelago, and even contribute to global history. Keywords: Lambanapu, prehistoric, Austronesian  Abstrak, Penelitian di Situs Lambanapu bertujuan untuk mengetahui posisi Lambanapu dalam persebaran dan perkembangan leluhur Austronesia dan budayanya di Sumba.  Metode yang dilakukan adalah survei, ekskavasi, analisis, dan interpretasi. Hasil penelitian berupa temuan rangka dan kubur tempayan serta artefak berupa gerabah, manik-manik, perhiasan logam, dan alat batu.  Dari hasil pertanggalan diketahui bahwa setidaknya Situs Lambanapu telah dihuni 2.000 tahun yang lalu. Hasil analisis paleoantropologi diperkirakan individu yang ditemukan di Lambanapu, baik kubur primer maupun sekunder, merupakan percampuran antara Mongoloid dan Australomelanesoid. Percampuran genetika memang sangat memungkinkan terjadi mengingat sejarah hunian Nusantara yang terisi oleh beberapa gelombang migrasi besar pada  masa lampau. Situs Lambanapu telah memberikan gambaran kehidupan leluhur Sumba dalam konteks Nusantara. Hasil penelitian memperlihatkan betapa Lambanapu dan Sumba pada umumnya memiliki kekayaan nilai sejarah dan budaya masa lampau yang sangat bermanfaat bagi kehidupan masa kini. Kekayaan nilai sejarah dan budayanya tidak hanya untuk kepentingan lokal, tetapi juga untuk mengisi kekayaan sejarah dan budaya Nusantara, bahkan kontribusi bagi sejarah global.  Kata kunci : Lambanapu, prasejarah, Austronesia
    Type of Medium: Online Resource
    ISSN: 2549-8908 , 0215-1324
    URL: Article
    DOI: 10.24832/amt.v36i2.67-80
    Language: Unknown
    Publisher: National Research and Innovation Agency
    Publication Date: 2018
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  • 2
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    Response to the comment by Huffman and Zaim
    Elsevier BV ; 2023
    In:  Quaternary Science Reviews Vol. 307 ( 2023-05), p. 108059-
    Details
    In: Quaternary Science Reviews, Elsevier BV, Vol. 307 ( 2023-05), p. 108059-
    Type of Medium: Online Resource
    ISSN: 0277-3791
    URL: Article
    DOI: 10.1016/j.quascirev.2023.108059
    RVK:
    RA 1000
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2023
    detail.hit.zdb_id: 780249-3
    detail.hit.zdb_id: 1495523-4
    SSG: 14
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  • 3
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    The Stegodon Bonebed of the Middle Pleistocene Archaeological Site Mata Menge (Flores, Indonesia): Taphonomic Agents in Site Formation
    MDPI AG ; 2021
    In:  Quaternary Vol. 4, No. 4 ( 2021-09-29), p. 31-
    Details
    In: Quaternary, MDPI AG, Vol. 4, No. 4 ( 2021-09-29), p. 31-
    Abstract: The Middle Pleistocene fluvial channel site of the Upper Fossil-bearing Interval at Mata Menge in the So’a Basin, Flores, Indonesia, has yielded the earliest fossil evidence for Homo floresiensis in association with stone artefacts and fossils of highly endemic insular fauna, including Stegodon, giant rats, crocodiles, Komodo dragons, and various birds. A preliminary taphonomic review of the fossil material here aimed to provide additional context for the hominin remains in this bonebed. Analysis was performed on two subsets of material from the same fluvial sandstone layer. Subset 1 comprised all material from two adjacent one-metre square quadrants (n = 91), and Subset 2 all Stegodon long limb bones excavated from the same layer (n = 17). Key analytical parameters included species and skeletal element identification; fossil size measurements and fragmentation; weathering stages; bone fracture characteristics; and other biological and geological bone surface modifications. Analysis of Subset 1 material identified a highly fragmented assemblage with a significant bias towards Stegodon. A large portion of these bones were likely fractured by trampling prior to entering the fluvial channel and were transported away from the death-site, undergoing surface modification causing rounding. Subset 2 material was less likely to have been transported far based on its limited susceptibility to fluvial transport. There was no significant difference in weathering for the long limb bones and fragments, with the highest portion exhibiting Stage 2 weathering, indicating that prior to final burial, all material was exposed to prolonged periods of surface exposure. Approximately 10% of all material have characteristics of fracturing on fresh bone, contributing to the taphonomic context for this bonebed; however insufficient evidence was found for anthropogenic modification.
    Type of Medium: Online Resource
    ISSN: 2571-550X
    URL: Article
    DOI: 10.3390/quat4040031
    Language: English
    Publisher: MDPI AG
    Publication Date: 2021
    detail.hit.zdb_id: 2934608-3
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  • 4
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    NEW FIND OF STEGODON SOMPOENSIS MAXILLA FROM CANGKANGE, SOPPENG, SOUTH SULAWESI
    Badan Standar, Kurikulum, dan Asesmen Pendidikan ; 2019
    In:  JURNAL WALENNAE Vol. 17, No. 2 ( 2019-12-13), p. 143-
    Details
    In: JURNAL WALENNAE, Badan Standar, Kurikulum, dan Asesmen Pendidikan, Vol. 17, No. 2 ( 2019-12-13), p. 143-
    Abstract: AbstractSulawesi is an island located in the Wallacean region of Indonesia. Geologically its lying midway between the Asian (Sunda) and Greater Australian (Sahul) continents. As a part of Wallacea islands, Sulawesi is an island that shows complexity either in biology or geology perspective. Though the distinctive quaternary vertebrate faunas has been described from Sulawesi, historical pattern of biogeography still poorly understood due to the lack of the fossil specimens. This paper describes a maxilla fragment with molar root teeth M1 from an archaic proboscidae called Stegodon that found in the conglomeratic sandstone layer, at Cangkange Area, 4 km to the east of Cabenge Archeological site of South Sulawesi, Indonesia. Based on the comparation measuring data between this specimen with the Stegodon sompoensis and the Stegodon trigonocephalus it can be concluded that this Stegodon maxilla fragment is belong to the Stegodon sompoensis, a dwarf Stegodon from Sulawesi Island. The specimen is a surface collected sample. Based on the attached matrix on the maxilla fragment, this specimen interpreted to be derived from subunit A of Beru Member, Walanae Formation. This Stegodon sompoensis is likely to be lived near the coastal-lagoon around 2,5 million years ago or Late Pliocene to Early Pleistocene. This estimated specimen age is based on the vertebrate fauna biostratigraphy of South Sulawesi. ABSTRAKPulau Sulawesi di Indonesia terletak di daerah Wallacea. Secara geologi pulau ini berada di antara Asia (paparan Sunda) dan Australia (paparan Sahul). Sebagai bagian dari kepulauan Wallacea, Pulau Sulawesi merupakan pulau yang memiliki kompleksitas baik dari segi biologi maupun geologinya. Meskipun fauna-fauna vertebrata kuarter Sulawesi sudah dideskripsi, tetapi sejarah dan pola biogeografi di pulau ini masih sangat kurang dikarenakan sedikitnya fosil-fosil yang ditemukan. Tulisan ini mendeskripsikan fragmen maxilla dari gajah purba jenis Stegodon dengan akar gigi molar M1 yang ditemukan di perlapisan batupasir konglomeratan, di daerah Cangkange, sekitar 4 km ke arah timur dari situs arkeologi Cabenge, Sulawesi Selatan, Indonesia. Berdasarkan perbandingan data pengukuran spesimen ini dengan Stegodon sompoensis dan Stegodon trigonocephalus maka disimpulkan bahwa fragmen maksila Stegodon ini berasal dari Stegodon sompoensis, jenis Stegodon kerdil dari Pulau Sulawesi. Spesimen ini merupakan temuan permukaan, tetapi berdasarkan matriks sedimen yang masih menempel di maxilla, spesimen ini diinterpretasikan berasal dari Anggota Beru subunit A. Stegodon sompoensis ini diperkirakan dahulu hidup di lingkungan lagoon dekat pantai pada sekitar 2,5 juta tahun yang lalu atau Pliosen Akhir sampai Pleistosen Awal. Penentuan umur ini didasarkan pada boistratigrafi fauna vertebrata Sulawesi Selatan.
    Type of Medium: Online Resource
    ISSN: 2580-121X , 1411-0571
    URL: Article
    DOI: 10.24832/wln.v17i2.366
    Language: Unknown
    Publisher: Badan Standar, Kurikulum, dan Asesmen Pendidikan
    Publication Date: 2019
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  • 5
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    Identifikasi Situs Geologi Cekungan Soa - Flores, Sebagai Salah Satu Warisan Geologi
    Pusat Air Tanah dan Geologi Tata Lingkungan, Badan Geologi ; 2021
    In:  Jurnal Lingkungan dan Bencana Geologi Vol. 12, No. 2 ( 2021-10-04), p. 83-94
    Details
    In: Jurnal Lingkungan dan Bencana Geologi, Pusat Air Tanah dan Geologi Tata Lingkungan, Badan Geologi, Vol. 12, No. 2 ( 2021-10-04), p. 83-94
    Abstract: ABSTRAK Cekungan Soa secara geografis terletak pada koordinat 80 39’ 00” LS - 80 46’ 00” LS dan 1210 03’ 00” BT - 1210 13’ 00” BT dan secara administratif terletak di Kabupaten Ngada dan Kabupaten Nagekeo, Pulau Flores, Nusa Tenggara Timur. Cekungan Soa memiliki keragaman geologi yang unik dan dapat dikembangkan menjadi destinasi geowisata yang menarik. Tujuan studi ini adalah untuk menginvetariasi keragaman geologi di Cekungan Soa, mengklasifikasikan peringkat nilai keragaman geologinya berdasarkan manfaatnya untuk selanjutnya dilakukan penilaian secara kuantitatif sebagai situs warisan geologi (geoheritage), dan merekomendasikan potensi situs warisan geologi tersebut untuk dikonservasi dalam bentuk Kawasan Cagar Alam Geologi (KCAG). Metode yang digunakan dalam studi ini berdasarkan “Standar teknis inventarisasi keragaman geologi dan Petunjuk Teknis Asesmen Sumberdaya Geologi” yang dikeluarkan oleh Pusat Survei Geologi pada tahun 2017. Ada 24 situs keragaman geologi di Cekungan Soa, yang memiliki peringkat nilai keragaman geologi menengah hingga terkemuka berdasarkan rekaman ilmiah dan fenomena geologi khusus untuk tujuan pendidikan maupun penelitian, sehingga pantas dijadikan sebagai geoheritage. Salah satunya adalah Situs Mata Menge yang memiliki nilai scientific sangat tinggi (91,25%). Dari hasil studi, kawasan Cekungan Soa direkomendasikan untuk dikonservasi menjadi KCAG.Kata kunci: Cekungan Soa, geowisata, keragaman geologi, warisan geologi, Kawasan Cagar Alam GeologiABSTRACT Soa Basin geographically situated at 80 39’ 00” S - 80 46’ 00” S and 1210 03’ 00” E - 1210 13’ 00” E in Ngada and Nagekeo District, Flores Island, East Nusa Tenggara. Soa Basin has unique geodiversity and can be developed into an interesting geotourism destination. This study aims to inventory the geological sites in the Soa Basin, to classify them as the geoheritage and to recommend them to be conserved in the form of Geoconservation Area (GCA). The method used in this study is based on the “Technical Standard of Geological Diversity Inventory and Technical Guidelines for Geological Resource Assessment” issued by the Geological Survey Center in 2017. There are 24 sites of geodiversities in the Soa Basin, which rank intermediate to prominent geological diversity values based on its scientific records and geological phenomena specifically for educational and research purposes, so the Soa Basin deserve to become as a geoheritage. Mata Menge, one of the site, has a very high scientific value of 91.25%. From the results of the assessment, it is recommended that the Soa Basin area be conserved as a GCA.Keywords: Soa Basin, geotourism, geodiversity, geoheritage, Geoconservation Are
    Type of Medium: Online Resource
    ISSN: 2502-8804 , 2086-7794
    DOI: 10.34126/jlbg.v12i2
    DOI: 10.34126/jlbg.v11i2.260
    Language: Unknown
    Publisher: Pusat Air Tanah dan Geologi Tata Lingkungan, Badan Geologi
    Publication Date: 2021
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  • 6
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    Depositional Environmental Changes of Cimanceuri Formation Based on Mollusk Fossil Assemblages in Bayah, Banten Province
    UIR Press ; 2019
    In:  Journal of Geoscience, Engineering, Environment, and Technology Vol. 4, No. 2 ( 2019-06-30), p. 66-
    Details
    In: Journal of Geoscience, Engineering, Environment, and Technology, UIR Press, Vol. 4, No. 2 ( 2019-06-30), p. 66-
    Abstract: Bayah is located in Lebak Regency, Banten Province. This location is chosen due to its abundant mollusk fossils which exposed along the outcrops. The aim of this research is to determine depositional environmental changes using mollusk fossil assemblages. Data obtained from a measured stratigraphic section of Cimanceuri Formation. It is dominated by very fine-fine sandstones with claystone intercalation.  A total thickness of measured stratigraphic section is 4.2 meters. There are at least seventeen mollusk associations (bottom-top) consisting of 1) Ringicula arctatoides - Olivella tomlini were obtained. 2) Ringicula arctatoides - Marginella (Cryptospira) ventricosa sangiranensis. 3) Olivella tomlini, 4) Ringicula arctatoides - Olivella tomlini, 5) Ringicula arctatoides, 6) Turritella (Turritella) bantamensis - Scapharca (Scapharca) gedinganensis, 7) Polinices aurantius - Marginella (Cryptospira) ventricosa sangiranensis, 8) Scapharca (Scapharca) gedinganensis, 9) Scapharca (Scapharca) multiformis - Timoclea bataviana, 10) Turritella (Turritella) bantamensis tjicumpaiensis - Ringicula arctatoides, 11) Turritella (Turritella) bantamensis - Ringicula arctatoides, 12) Turritella (Turritella) bantamensis tjicumpaiensis - Turritella (Turritella) bantamensis, 13) Turritella (Turritella) bantamensis tjicumpaiensis - Ringicula arctatoides, 14) Turritella (Turritella) bantamensis - Architectonica sp., 15) Turritella (Turritella) bantamensis tjicumpaiensis, 16) Turritella (Turritella) bantamensis – Turritella (Turritella) bantamensis tjicumpaiensis, and 17) Turritella (Turritella) bantamensis. The condition with the most stable ecosystem is the association of Turritella (Turritella) bantamensis tjicumpaiensis - Turritella (Turritella) bantamensis (Association 12). At least there are seven depositional environmental changes that occur in this research area with two shallowing – deepening cycles : 1) open shallow marine, 2) subtidal – open shallow marine, 3) open shallow marine, 4) open shallow marine – subtidal, 5) subtidal, 6) subtidal – open shallow marine, and 7) open shallow marine.
    Type of Medium: Online Resource
    ISSN: 2541-5794 , 2503-216X
    URL: Issue
    URL: Article
    DOI: 10.25299/jgeet.2019.4.2
    DOI: 10.25299/jgeet.2019.4.2.2986
    Language: Unknown
    Publisher: UIR Press
    Publication Date: 2019
    detail.hit.zdb_id: 3069706-2
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  • 7
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    Teknologi Litik di Situs Talimbue, Sulawesi Tenggara: Teknologi Berlanjut dari Masa Pleistosen Akhir Hingga Holosen.
    National Research and Innovation Agency ; 2016
    In:  AMERTA Vol. 34, No. 2 ( 2016-12-01), p. 81-
    Details
    In: AMERTA, National Research and Innovation Agency, Vol. 34, No. 2 ( 2016-12-01), p. 81-
    Abstract: Abstract.  The  Lithic  Technology  at  Talimbue  Site,  Southeast  Sulawesi:  Continuing  Technology from Late Pleistocene up to Holocene Periods. The Talimbue site at Southeast Sulawesi is packed with  lithic  and  these  offer  a  new  perspective  on  the  lithic  technology  of  Sulawesi.  The  absence  of information  on  the  prehistoric  lithic  technology  of  Southeast  Sulawesi  is  a  factor  of  interest  that makes  research  on  knowledge  of  the  Talimbue  site  necessary.  Lithic  artefacts  were  manufactured from  the  terminal  Pleistocene  to  the  Late  Holocene.  This  research  will  disentangle  the  details  of the lithic technology at the Talimbue Site. The analyzed flaked stone artefacts fall into 3 categories, which are retouched flakes, debitage and cores. For its part, debitage was classified into 3 categories, which are complete flakes, broken flakes and debris. The retouch index was also measured so as to provide a quantitative estimate of the level of retouch intensity of the retouched flakes. The results of  the  analysis  indicate  changes  in  the  stone  flake  technology  during  the  period  of  occupation  of the Talimbue Site. The change of technology occurs because the process of adaptation caused by a change of environment. Abstrak. Temuan  litik  yang  sangat  padat  di  Situs  Talimbue  di  Sulawesi  Tenggara  menunjukkan sebuah persepektif baru dalam kajian teknologi litik di Sulawesi. Kekosongan informasi teknologi litik masa prasejarah di wilayah Sulawesi Tenggara adalah hal yang menarik dikaji dalam penelitian di Situs Talimbue. Artefak litik digunakan dari masa Pleistosen Akhir hingga masa Holosen Akhir. Penelitian ini akan menguraikan secara detail bagaimana teknologi litik di Situs Talimbue. Artefak batu diserpih yang dianalisis menjadi 3 kategori, yaitu serpih diretus, serpihan dan batu inti. Serpihan kemudian  diklasifikasi  menjadi  3  kategori,  yaitu  serpih  utuh,  serpih  rusak  dan  tatal.  Pengukuran indeks retus juga dilakukan bertujuan untuk mengestimasi secara kuantitatif tingkat intensitas retus terhadap serpih yang telah diretus. Hasil penelitian menunjukkan perubahan teknologi artefak batu diserpih terjadi selama masa hunian di Situs Talimbue. Perubahan teknologi terjadi karena adanya proses adaptasi yang disebabkan oleh perubahan lingkungan.
    Type of Medium: Online Resource
    ISSN: 2549-8908 , 0215-1324
    URL: Article
    DOI: 10.24832/amt.v34i2.146
    Language: Unknown
    Publisher: National Research and Innovation Agency
    Publication Date: 2016
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  • 8
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    Vestige of The Ancient Estuarine of Cisaar Valley, Sumedang as One of the Pleistocene Fossil Bearing Site in West Jawa
    National Research and Innovation Agency ; 2019
    In:  PURBAWIDYA: Jurnal Penelitian dan Pengembangan Arkeologi Vol. 8, No. 2 ( 2019-11-29), p. 65-80
    Details
    In: PURBAWIDYA: Jurnal Penelitian dan Pengembangan Arkeologi, National Research and Innovation Agency, Vol. 8, No. 2 ( 2019-11-29), p. 65-80
    Abstract: Cisaar Valley is located on the east part of Sumedang Regency, West Jawa Province. It’s close to the boundary of Sumedang-Majalengka Regency. In this location the sandy and clay dominated sedimentary rocks are well exposed along the outcrops in the Cisaar Valley. These sedimentary rocks is inferred from Pliocene-Pleistocene deposits from Kaliwangu and Citalang Formation. Foraminifera microfossil that commonly used for interpretation of depositional environment is rarely found, whereas freshwater mollusk and vertebrate fossils often found in the sediment rocks of this area.  This condition raises a question, what is the environment of this valley in the past? Data obtained from measured stratigraphic sections along Cisaar river and its tributary rivers in Cibengkung and Cirendang hamlets, Jembarwangi village. There are at least three depositional paleoenvironments which from old to young are: shallow marine, estuarine and fluviatil braided channel depositional paleoenvironment.  Characteristics of the lower, middle and upper of the estuarine environment were found in this Cisaar Valley as the evidences of the oceanic regression processes was happened in the past in this area. 
    Type of Medium: Online Resource
    ISSN: 2528-3618 , 2252-3758
    URL: Article
    DOI: 10.24164/pw.v8i2.302
    Language: Unknown
    Publisher: National Research and Innovation Agency
    Publication Date: 2019
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  • 9
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    When did Cuon reach Java? – Reinvestigation of canid fossils from Homo erectus faunas
    Elsevier BV ; 2019
    In:  Geobios Vol. 55 ( 2019-09), p. 89-102
    Details
    In: Geobios, Elsevier BV, Vol. 55 ( 2019-09), p. 89-102
    Type of Medium: Online Resource
    ISSN: 0016-6995
    URL: Article
    DOI: 10.1016/j.geobios.2019.06.004
    RVK:
    TE 1000
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2019
    detail.hit.zdb_id: 2098288-4
    SSG: 13
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  • 10
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    Palaeoenvironments and palaeontology of the Atambua Basin, West Timor, Indonesia
    Elsevier BV ; 2021
    In:  Quaternary International Vol. 603 ( 2021-11), p. 82-89
    Details
    In: Quaternary International, Elsevier BV, Vol. 603 ( 2021-11), p. 82-89
    Type of Medium: Online Resource
    ISSN: 1040-6182
    URL: Article
    DOI: 10.1016/j.quaint.2021.01.023
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2021
    detail.hit.zdb_id: 2002133-1
    detail.hit.zdb_id: 1077692-8
    SSG: 13
    SSG: 14
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