ライフサイエンスコーパス: montane

1 In the lower montane and lowland zones simulated ecosystem productivi

2 er levels of ERalpha-IR in the MeA than male montane and meadow voles and in the BST relative to mont

3 eaf wetting patterns in contrasting tropical montane and pre-montane cloud forests.

4 er uptake differed significantly between the montane and pre-montane forest plant communities, as wel

5 er dominated discharge year-round across the montane and urban sites, challenging the conceptual emph

6 tly low during snowmelt and baseflow in most montane and urban stream reaches, indicating effective s

7 ground biomass in both lowland Amazonian and montane Andean landscapes.

8 ome lineages colonized lowlands and adjacent montane areas, but diversification in those areas remain

9 d of extinction and 'evolutionary rescue' in montane biodiversity hot spots under climate change scen

10 Epiphytes are common in tropical montane cloud forests (TMCFs) and play many important ec

11 Tropical montane cloud forests (TMCFs) depend on predictable, fre

12 Tropical montane cloud forests (TMCFs) harbour high levels of bio

13 et of "optimal" climatic conditions found in montane cloud forests is similar to that of maritime tem

14 ecognisable and defining feature of tropical montane cloud forests, little research has focussed on h

15 erns in contrasting tropical montane and pre-montane cloud forests.

16 tructure, diversity, and spatial turnover of montane communities in a phylogenetic context.

17 of the area currently capable of supporting montane conifer forest could become subject to minimal c

18 Oregon, where severe fire initially converts montane conifer forests to systems dominated by broadlea

19 ades across the climatic aridity gradient of montane conifer forests.

20 and beetle body temperature (T(b)) in three montane drainages in the Sierra Nevada, California.

21 xploited potential for studying responses of montane ecosystems to temperature and predicting phenolo

22 ing may disrupt the functional properties of montane ecosystems, particularly where plant community r

23 n drive the evolution of nutrient budgets in montane ecosystems, with implications for predicting for

24 have consequences for amphibians inhabiting montane ecosystems.

25 d strong FA of low-elevation perennials in a montane environment.

26 explain FA of low-elevation perennials in a montane environment.

27 Montane environments around the globe are biodiversity '

28 climatic zones along elevation gradients in montane environments.

29 humid forests of northwest Madagascar and a montane ericoid formation of the central highlands show

30 Nevada, implying that the risk of increasing montane ET with warming is widespread.

31 previously considered to primarily use moist montane forest during the winter, but this seems unlikel

32 ere we show that dust may also be crucial in montane forest ecosystems, dominating nutrient budgets d

33 the Northern Hemisphere occurs in seasonal, montane forest ecosystems.

34 We developed a method to model and map the montane forest ecotone using Landsat imagery to observe

35 During the dry season, the montane forest experienced higher precipitation, cloud c

36 e from Ecuador reveals the response of lower montane forest on the Andean flank in western Amazonia t

37 ed significantly between the montane and pre-montane forest plant communities, as well as among speci

38 anda has been restricted to several disjunct montane forest populations, and habitat loss and fragmen

39 aleoecological record from Neotropical lower montane forest reveals a consistent forest presence and

40 tting events of longer duration than the pre-montane forest.

41 included primary and secondary-growth lower montane forests (500-1.200 m above sea level) and primar

42 r, in some cases similar to the most fertile montane forests in the Hawaiian Islands.

43 n a very remote area, suggests that tropical montane forests may contain greater AGB than previously

44 hytic species distributed in lowland and pre-montane forests of Central and South America.

45 a dioecious neotropical tree common in lower montane forests of Monteverde, Costa Rica.

46 fied forest soils and freshwaters throughout montane forests of the northeastern United States; the r

47 Montane forests of western China provide an opportunity

48 cause shifts in the composition of tropical montane forests towards increased relative abundances of

49 Upper montane forests were predicted to allocate ~50% of carbo

50 In lower montane forests, regardless of land-use history, we foun

51 In lowland to montane forests, three invasive tree species replace nat

52 arp transition in NPP between submontane and montane forests, which may be caused by cloud immersion

53 tant drivers of atmospheric Hg deposition to montane forests.

54 n disturbance by fire and forest thinning in montane forests.

55 rtia to climatically induced range shifts in montane forests; the upslope shift may have been acceler

56 kely to promote population viability in this montane frog population.

57 e than 16,500 terrestrial vertebrates on 180 montane gradients.

58 Reconstruction of the distribution of a montane grasshopper species during the last glacial maxi

59 km yr(-1)), temperate coniferous forest, and montane grasslands.

60 a trend towards LA among populations within montane habitats.

61 enetic structure of populations of an arctic-montane herb, Saxifraga hirculus (Saxifragaceae), was an

62 elative contributions of these mechanisms to montane invasion resistance, yet such experiments are ra

63 the importance of these factors in limiting montane invasions using a field transplant experiment ab

64 Interpretation of tropical-montane isotope records is controversial, especially con

65 -y period (1949/1951-2007/2009) in a complex montane landscape (the Siskiyou Mountains, Oregon) where

66 Montane landscapes may effectively shelter many species

67 and meadow voles and in the BST relative to montane males.

68 three species of microtines, the polygynous montane (Microtus montanus) and meadow (M. pennsylvanicu

69 hese patterns are explained by greater time (montane museum) rather than faster speciation at mid-ele

70 utterflies overwinter in restricted areas in montane oyamel fir forests in central Mexico with specif

71 tic Hawaiian group to two diploid species of montane perennial herbs in California, Madia bolanderi a

72 The altitudinal shifts of many montane populations are lagging behind climate change.

73 nces among PGI genotypes, which suggest that montane populations of this beetle are locally adapted t

74 emistry of forest canopies across a Hawaiian montane rain forest landscape.

75 argeted conservation measures, especially of montane refuge populations, may yet preserve a represent

76 earing climates are concentrated in tropical montane regions and the poleward portions of continents.

77 is distributed predominantly across arid and montane regions of Asia.

78 self-fertilizing species occurring in mostly montane regions of western North America.

79 Montane regions worldwide have experienced relatively lo

80 In montane regions, where climate change is expected to cau

81 e can all strongly affect plant invasions in montane regions.

82 prolite assemblage from a rock overhang in a montane river valley in southern New Zealand.

83 the study presented here, genetic data from montane scorpions in the Vaejovis vorhiesi group, restri

84 y estimating the potential distribution of a montane shrew (Mammalia, Soricidae, Cryptotis mexicanus)

85 Montane species are also typically more vulnerable to en

86 The imminent demise of montane species is a recurrent theme in the climate chan

87 ding that average upslope shifts in tropical montane species match local temperature increases signif

88 er than faster speciation at mid-elevations (montane species pump), despite the recency of the major

89 ficantly more closely than in temperate-zone montane species.

90 ons and are most prevalent among Neotropical montane, stream-associated species.

91 (Baetis bicaudatus and B. tricaudatus) from montane streams over an elevation gradient spanning 1400

92 t dominates the hydrograph of many temperate montane streams, yet little work has characterized how s

93 s using two AF social wasp species - the mid-montane Synoeca cyanea and the lowland Synoeca aff.

94 s may be relevant to other Andean clades and montane systems globally.

95 ing temperature with increasing elevation in montane systems has long been recognized as a major fact

96 0-1.200 m above sea level) and primary upper montane to subalpine forests (1,500-2,100 m above sea le

97 establishment ability of subalpine and upper montane trees.

98 minance of the tree, Oreomunnea mexicana, in montane tropical forest in Panama.

99 t not in the relatively asocial, promiscuous montane vole.

100 romiscuous vole species, the meadow vole and montane vole.

101 voles (Microtus ochrogaster) and promiscuous montane voles (Microtus montanus) exhibit remarkable dif

102 differently in infant and adult prairie and montane voles and, thus, could exert differential effect

103 AVP receptor binding showed an early peak in montane voles but did not change significantly in prairi

104 Male and female montane voles did not differ.

105 ult level at weaning, whereas the binding in montane voles remained unchanged into adulthood.

106 ad higher AVP receptor binding at birth than montane voles, and this difference persisted with little

107 Thereafter, the binding increased rapidly in montane voles, but it remained unchanged in prairie vole

108 ained 5.2 degrees C MAT gradient in tropical montane wet forests on the Island of Hawaii.

109 and distribution of carbon pools in tropical montane wet forests will be less sensitive to rising MAT

110 individuals of the forest bird species, the Montane White-eye Zosterops poliogaster from 16 sites an

111 In the upper montane zone the model predicted a lack of forest vegeta