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Kabupaten Nias Selatan

Badan Riset dan Inovasi Nasional

Informasi Dataset

07-11-2022

13-08-2024

73b80e12-3bd2-487b-9d23-4fe07836a079

Dataset Serupa
Contrasting Patterns of Growth and Migration of Tropical Anguillid Leptocephali ...

In order to improve understanding of the larval migration and early life history...

Habitat Characteristics of Lake Towuti, South Sulawesi, Indonesia-The Home of En...

The aim of this study was to examine the habitat characteristic features of Lake...

Habitat Characteristics of Carsinofauna and Mollucifauna in Towuti Lake, South S...

Lake Towuti is a tectonic-oligotrophic lake that located in Malili Complex, Sout...

Late 20th century warming and and freshening in the central tropical Pacific

Global climate models and analyses of instrumental datasets provide a wide range...

The importance of the Banda Sea for tuna fisheries : A review of studies on the ...

Tuna exploitation in the Banda Sea has been started when Indonesia government ga...

INFORMASI: Data berikut ini masih dalam proses pemenuhan Prinsip SDI.

The Towuti Drilling Project: Paleoenvironments, Biological Evolution, And Geomicrobiology Of A Tropical Pacific Lake

Terbatas

The Towuti Drilling Project (TDP) is an international research program, whose goal is to understand long-term environmental and climatic change in the tropical western Pacific, the impacts of geological and environmental changes on the biological evolution of aquatic taxa, and the geomicrobiology and biogeochemistry of metal-rich, ultramafic-hosted lake sediments through the scientific drilling of Lake Towuti, southern Sulawesi, Indonesia. Lake Towuti is a large tectonic lake at the downstream end of the Malili lake system, a chain of five highly biodiverse lakes that are among the oldest lakes in Southeast Asia. In 2015 we carried out a scientific drilling program on Lake Towuti using the International Continental Scientific Drilling Program (ICDP) Deep Lakes Drilling System (DLDS). We recovered a total of  ∼ 1018 m of core from 11 drilling sites with water depths ranging from 156 to 200 m. Recovery averaged 91.7  persen, and the maximum drilling depth was 175 m below the lake floor, penetrating the entire sedimentary infill of the basin. Initial data from core and borehole logging indicate that these cores record the evolution of a highly dynamic tectonic and limnological system, with clear indications of orbital-scale climate variability during the mid- to late Pleistocene. Scientific Drilling, Vol. 21. 2016. P: 29-40

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