Institution
Indonesian Institute of Sciences
Facility•Jakarta, Indonesia•
About: Indonesian Institute of Sciences is a facility organization based out in Jakarta, Indonesia. It is known for research contribution in the topics: Population & Genus. The organization has 4795 authors who have published 10544 publications receiving 76990 citations. The organization is also known as: Indonesian Institute of Sciences Cibinong, Indonesia.
Topics: Population, Genus, Species richness, Fermentation, Biodiversity
Papers published on a yearly basis
Papers
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TL;DR: In this article, an analysis of coral rings grown in the interval 1970-1997 reveals a geographically distinct pattern of interseismic uplift off Sumatra's western coast. And they suggest that a locked, or partially locked patch, located above 30 km depth on the upper surface of the subducting oceanic plate, generates this pattern.
Abstract: Analyses of coral rings grown in the interval 1970–1997 reveal a geographically distinct pattern of interseismic uplift off Sumatra's western coast. At distances less than 110 km from the Sumatran trench, coral reefs are submerging as fast as 5 mm/y. At 130 and 180 km distance from the trench, they are emerging at similar rates. We suggest that a locked, or partially locked patch, located above 30 km depth on the upper surface of the subducting oceanic plate, generates this pattern.
85 citations
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TL;DR: In this article, five new resveratrol oligomers; pauciflorols A, C, B, isovaticanols B and C (8), and three new oligostilbene glucosides; paupliflorosides A (11), B (13), C (14), and C(15), were isolated from the stem bark of Vatica paucifera (Dipterocarpaceae) together with known 17 resveraratrol oligomer (4, 5, 7, 9, 10, 12 and
85 citations
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85 citations
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TL;DR: A 2,000-year, multiproxy reconstruction of western Pacific hydroclimate from two speleothem records for southeastern Indonesia highlights the likelihood that century-scale variations in tropical Pacific climate modes can significantly modulate radiatively forced shifts in global temperature.
Abstract: Australian Research Council Discovery [DP0663274, DP1095673]; NOAA/UCAR Climate and Global Change Postdoctoral Fellowship; William Paterson University; Lewis and Clark College Mellon Research Initiative Fellowship; US NSF
85 citations
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TL;DR: The first barrier encountered by Pacific water directed towards Makassar Strait is the 1350-m deep Sangihe Ridge, providing access to the Sulawesi Sea.
Abstract: Whereas at the surface and at thermocline depth the Indonesian throughflow can weave its way between basins towards the Indian Ocean on a quasi-horizontal plane, at greater depth numerous sills are encountered, resulting in circulation patterns governed by density-driven overflow processes. Pacific water spills over deep topographic barriers into the Sulawesi Sea and into the Seram and Banda seas. The western-most throughflow path flowing through Makassar Strait encounters shallower barriers than does the eastern path. The first barrier encountered by Pacific water directed towards Makassar Strait is the 1350-m deep Sangihe Ridge, providing access to the Sulawesi Sea. The 680-m deep Dewakang Sill separating the southern Makassar Strait from the Flores Sea is a more formidable barrier. Along the eastern path, Pacific water must flow over the 1940 m barrier of the Lifamatola Passage before passing into the deep levels of the Seram and Banda Seas. The deepest barrier encountered by both the western and eastern paths to the Indian Ocean is the 1300–1450 m (perhaps as deep as 1500 m) sill of the Sunda Arc near Timor. The Savu Sea while connected to the Banda Sea down to 2000 m depth, is closed to the Indian Ocean at a depth shallower than the Timor Sill. The density-driven overflows force upwelling of resident waters within the confines of the basins, which is balanced by diapycnal mixing, resulting in an exponential deep-water temperature profile. A scale depth (Z*=Kz/w) of 420–530 m is characteristic of the 300–1500 m depth range, with values closer to 600 m for the deeper water column. The upwelled water within the confines of the Banda Sea, once over the confining sill of the Sunda Arc, may contribute 1.8–2.3 Sv the interocean throughflow.
84 citations
Authors
Showing all 4828 results
Name | H-index | Papers | Citations |
---|---|---|---|
Katsumi Tsukamoto | 63 | 415 | 14099 |
Munekazu Iinuma | 51 | 436 | 11236 |
Jun Aoyama | 37 | 133 | 4174 |
Danny H. Natawidjaja | 34 | 109 | 5306 |
Tetsuro Ito | 32 | 108 | 3196 |
Toshiyuki Tanaka | 31 | 162 | 4356 |
Teruhiko Yoshihara | 31 | 125 | 2952 |
Leonardus B.S. Kardono | 29 | 80 | 2424 |
Suharyo Sumowidagdo | 27 | 100 | 2208 |
Bambang W. Suwargadi | 27 | 59 | 3072 |
Mark V. Erdmann | 27 | 110 | 3074 |
Ahmad Fudholi | 26 | 173 | 3311 |
Wahyoe S. Hantoro | 26 | 56 | 3296 |
Muhammad Danang Birowosuto | 25 | 123 | 2061 |
Kosaku Takahashi | 25 | 80 | 1867 |