ライフサイエンスコーパス: Sumatra

1 associated with future land use scenarios in Sumatra.

2 a major contributor to natural disasters in Sumatra.

3 status given to the remaining peatswamps on Sumatra.

4 he living orang-utan (Pongo) from Borneo and Sumatra.

5 en the west coast of Peninsular Malaysia and Sumatra.

6 ed cats and male domestic cats on Borneo and Sumatra.

7 tan and 5 gibbon individuals from Borneo and Sumatra.

8 ) and limited to a localized area in Central Sumatra (1.6% of Indonesia): burning an estimated 163,33

9 Toba, Sumatra, 75,000 y ago, which produced voluminous ash dep

10 and southeast Asia, including the islands of Sumatra and Borneo in the Indonesian archipelago.

11 The populations on Sumatra and Borneo instead show low inbreeding, but high

12 tricted to small and isolated populations on Sumatra and Borneo, and most likely extinct on the Malay

13 ses on the three extant orangutan species of Sumatra and Borneo, our findings have broad application

14 bes the southeast Asian great apes native to Sumatra and Borneo.

15 al models suggest that these frogs colonized Sumatra and diversified on the island before the occurre

16 nups of up to 13 m on the adjacent coasts of Sumatra and Java.

17 Longer-term records of airport visibility in Sumatra and Kalimantan show that 2015 ranked after 1997

18 r DNA from orang-utans from two locations in Sumatra and nine locations-representing four isolated po

19 land management on the Indonesian island of Sumatra and the sensitivity of this fire activity to int

20 the plate boundary offshore of northwestern Sumatra and the southern Nicobar islands.

21 (i.e., on the continental mainland, Borneo, Sumatra, and Java), each morphospecies was generally wel

22 d animals, than in the Sunda Region (Borneo, Sumatra, and Peninsular Malaysia), with a highly diverse

23 inent brushed up against the western side of Sumatra, and the other two events occurring as India mov

24 rsity in isolation, corridors (Java, Maluku, Sumatra, and the Thai-Malay Peninsula) connect neighbori

25 The 2004 Sumatra-Andaman and 2011 Tohoku-Oki earthquakes highligh

26 The human tragedy caused by the Sumatra-Andaman earthquake (moment magnitude 9.3) on 26

27 ic events, namely the 2004 magnitude (M) 9.1 Sumatra-Andaman earthquake and the earlier 1992 M = 7.3

28 The great Sumatra-Andaman earthquake and tsunami of 2004 was a dra

29 trength changes produced by the distant 2004 Sumatra-Andaman earthquake are especially important, as

30 of other great earthquakes indicate that the Sumatra-Andaman earthquake did indeed have a moment magn

31 Swedish survivors of tsunamis from the 2004 Sumatra-Andaman earthquake had increased risks of psychi

32 owing the massive loss of life caused by the Sumatra-Andaman earthquake in Indonesia and its tsunami,

33 The 26 December 2004 Sumatra-Andaman earthquake initiated slowly, with small

34 The disastrous Sumatra-Andaman earthquake of 26 December 2004 was one o

35 results reveal that Indonesia's devastating Sumatra-Andaman earthquake on 26 December 2004 was 2.5 t

36 as contiguous with that of the December 2004 Sumatra-Andaman earthquake, and is likely to have been s

37 of 9.0 was obtained several hours after the Sumatra-Andaman earthquake, but more recent, longer-peri

38 ccurring in the few years following the 2004 Sumatra-Andaman earthquake.

39 ty change induced by the great December 2004 Sumatra-Andaman earthquake.

40 edge of the 2005 rupture from the great 2004 Sumatra-Andaman rupture.

41 Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to

42 Shallow slip offshore Sumatra appears driven by diagenetic strengthening of de

43 The Toba supereruption in Sumatra, approximately 74 thousand years (ka) ago, was t

44 corded by continuous geodetic stations along Sumatra as the result of water- and stress-activated cre

45 Ocean pathway of the ITF was discovered off Sumatra associated with prolonged northwestward flow wit

46 c "supereruption" of the Mount Toba volcano (Sumatra) at approximately 74,000 y before present (B.P.)

47 ethods used to easily discriminate Siam from Sumatra balsam (also known as Benzoe sumatranus Indonesi

48 g of mammalian teeth, place modern humans in Sumatra between 73 and 63 ka.

49 of up to 15 meters occurred near Banda Aceh, Sumatra, but to the north, along the Nicobar and Andaman

50 ~ 0.4-0.5 in the offshore region of the west Sumatra Coast in the east IOD zone, while it increased t

51 Here, the 5 year flood record for Sumatra derived from governmental reports, as well as fr

52 The 2004 M = 9.2 Sumatra earthquake altered seismicity in the Andaman bac

53 bservations of the 2012 moment magnitude 8.6 Sumatra earthquake reveal unprecedented complexity of dy

54 ty over a large area associated with 3 major Sumatra earthquakes in 2004, 2005, and 2007.

55 We find ~80% of 2005-2009 Sumatra emissions are associated with degradation or lan

56 study area, we predict that 37-48% of future Sumatra emissions from land use change will occur in fue

57 as on the neighbouring, vertical strike-slip Sumatra fault, and find an increase in stress on both st

58 expanded the area of increased stress on the Sumatra fault.

59 We also found that in Sumatra, few lowland forests remained, suggesting that a

60 We estimate Sumatra fire emissions from land use change and maintena

61 tracted from corals of the Mentawai islands, Sumatra, imply that this 700-kilometer-long section of t

62 Sunda region (with a focus on the island of Sumatra) in shaping the evolutionary history of two gene

63 p of the Sunda megathrust, offshore northern Sumatra, in March 2005.

64 e in several parts of the back-arc region of Sumatra, in the opposite direction to the NNE subduction

65 esults of a large-scale restoration trial in Sumatra (Indonesia), monitored for 7.5 years.

66 d-based programs, a study was carried out in Sumatra, Indonesia, of the effect of food sources of bet

67 eflection profiles across the trench west of Sumatra, Indonesia, show differences across the boundary

68 presenting land-cover-change trajectories in Sumatra, Indonesia.

69 s in tropical rainforests and plantations in Sumatra, Indonesia.

70 ia from three Pleistocene cave localities in Sumatra, Indonesia.

71 g of energy through soil animal food webs in Sumatra, Indonesia.

72 two land-cover types in tropical peatland in Sumatra, Indonesia: (a) a natural forest and (b) an Acac

73 egrees S-5 degrees N) and the region off the Sumatra-Java coast (SJC: 100 degrees E-110 degrees E, 13

74 ously easterly winds along the southern Java-Sumatra occurs several weeks before the GWL drop to the

75 h are located in Borneo (P. p. pygmaeus) and Sumatra (P. p. abelii), respectively.

76 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within

77 stematic sign transects, and camera traps in Sumatra's largest remaining tropical forest and used int

78 ed about 100-200 kilometres southwest of the Sumatra subduction zone.

79 neo (subspecies Pongo pygmaeus pygmaeus) and Sumatra (subspecies P. p. abelii).

80 aves from the 26 December 2004 earthquake in Sumatra swept across Alaska, they triggered an 11-minute

81 h shallow lapse rates; for example, northern Sumatra, the Brazilian highlands and southern Africa.

82 slab pull stresses as the plate underthrusts Sumatra to the northeast.

83 propagation patterns of the 26 December 2004 Sumatra tsunami were primarily determined by the orienta

84 he possible existence of back-arc thrusts in Sumatra, we examine regional earthquake data reported by

85 the extent of the inundation in Banda Aceh, Sumatra, were combined with satellite imagery to quantif

86 econstructed rainfall changes over Northwest Sumatra (western IPWP, Indian Ocean) throughout the past

87 whether such back-arc thrust faults exist in Sumatra, which is located in the western part of the Sun

88 wider sampling of N. n. diardi in Borneo and Sumatra, would support reclassification of N. n. diardi