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1 bles, on ecosystem dynamics in a subtropical rainforest.
2 it-scarce periods in a West African tropical rainforest.
3 ation ranging from wooded savannahs to humid rainforest.
4 CO2), with highest levels in rivers draining rainforest.
5 tions located west-to-east of the equatorial rainforest.
6 anging from cool Andean highland to Amazonia rainforest.
7 he earliest megafossil record of Neotropical rainforest.
8 -scale "dieback" or degradation of Amazonian rainforest.
9 lar family composition to extant Neotropical rainforest.
10 nitrogen and volatile organic compounds than rainforest.
11 large tracts of commercially logged tropical rainforest.
12 em due to deforestation only of parts of the rainforest.
13 non-ENSO year 2000 in a Costa Rican tropical rainforest.
14 heir unique lifestyle in the Central African rainforest.
15 in the photochemistry active over the Amazon rainforest.
16 ree Pacific coast to the VBRV-endemic Amazon rainforest.
17 triggers tree death from drought in tropical rainforest.
18 ion experiment (TFE) in an eastern Amazonian rainforest.
19 ersity over 8-16 years in eight successional rainforests.
20 r of avian speciation in lowland Neotropical rainforests.
21 al ecosystem processes dominated by tropical rainforests.
22 ose clades that succeeded radiating into the rainforests.
23 in few animal-pollinated plants in tropical rainforests.
24 N in stream waters of temperate and tropical rainforests.
25 od shortages in their native Southeast Asian rainforests.
26 pproximately 25% in a majority of the Amazon rainforests.
27 corridor between the Amazonian and Atlantic rainforests.
28 s similar to the litter of extant equatorial rainforests.
29 matic events pose severe hazards to tropical rainforests.
30 reme heat and drought over most of Amazonian rainforests.
31 t role in the redistribution of nutrients in rainforests.
32 n shape community dynamics in highly diverse rainforests.
33 se are limiting factors in coastal temperate rainforests.
34 is roughly equivalent to that of terrestrial rainforests.
35 ese ecological processes operate in tropical rainforests.
37 of large geometric earthworks beneath intact rainforest across southern Amazonia challenges its statu
38 seen in a set of well characterized Hawaiian rainforests, across which we have measured the 15N/14N o
40 arts of the boreal forest belt, the tropical rainforest, alpine regions worldwide, steppe and prairie
41 centrations do not differ significantly over rainforest and adjacent oil palm plantation landscapes.
42 berg rock outcrops in the Brazilian Atlantic rainforest and are thus long-term fragmented by nature.
44 rns, which occupies the junction between the rainforest and dry forest and currently is known only fr
46 af-litter ant species in unlogged and logged rainforest and tested four predictions: (i) there is a n
47 e the nonlinear couplings between the Amazon rainforest and the atmospheric moisture transport from t
48 ve compass information for navigation in the rainforest and, additionally, provide cues for visual di
49 te the theory: bird conservation in tropical rainforests and coastal defence provided by mangrove for
51 s collected over three decades, we show that rainforest anthrax is a persistent and widespread cause
54 94 out of every 100 individual arthropods in rainforests are ants, and they constitute up to 15% of a
55 future climate and fire conditions: tropical rainforests are especially vulnerable, whereas seasonal
56 topographic positions suggests that tropical rainforests are more sensitive to moisture deficits than
63 ammalian diversity distributions, one in the rainforest areas (Deep Rainforest Diversity, DRD) contai
64 damped driven pendulum, a model of Amazonian rainforest as a known climate tipping element and the Da
65 vey of 49 ecosystems from tundra to tropical rainforest, average worker mass and worker number were u
66 olution experiment conducted in the tropical rainforest, bats visited computer-automated flowers with
67 irst moved southward, through the equatorial rainforest, before spreading toward eastern and southern
68 s have been logged, with dramatic impacts on rainforest biodiversity that may disrupt key ecosystem p
69 at outbreaks located along the limits of the rainforest biome were significantly associated with fore
71 esponds strongly to conversion of the Amazon rainforest, but in a manner different from plants and an
74 were slowed, delaying the occupation of the rainforest by on average 300 y, compared with similar mi
75 extraordinary abundance of ants in tropical rainforest canopies has led to speculation that numerous
76 rophic 50-foot free-fall from the top of the rainforest canopy to the forest floor at her remote fiel
85 ries under terra firme (upland interfluvial) rainforest, directly challenging the "pristine" status o
86 clude that the wet periods probably affected rainforest distribution, as plant fossils show that fore
87 rsity occurred at the same time as a loss of rainforest diversity and cannot be explained by ecologic
89 ributions, one in the rainforest areas (Deep Rainforest Diversity, DRD) containing taxa of lower hunt
91 e related to differential losses of tropical rainforests during the Cenozoic, but not to the cumulati
92 lar, the hypothesized replacement of ancient rainforest-dwelling extinct lineages by antecedents of x
93 This work demonstrates that while temperate rainforest dynamics occur at fine spatial scales (<1000
95 The impacts of this climate extreme on the rainforest ecosystems remain to be documented and are li
96 of these epiphytes--a neglected component in rainforest ecosystems--can more than double our estimate
98 biomass of invertebrates living in a common rainforest epiphyte, describe a striking relationship be
101 over the late Quaternary period by modeling rainforest expansion and contraction in 21 biogeographic
102 r settlement despite the climatically driven rainforest expansion that began approximately 2,000 y ag
103 de strong evidence that the same Neotropical rainforest families have characterized the biome since t
104 r is a Sumatran Pleistocene cave with a rich rainforest fauna associated with fossil human teeth.
105 f ants to the removal of food resources from rainforest floors and thus nutrient redistribution.
106 t all tropical fruits are equally desired by rainforest foragers and some fruit trees get depleted mo
107 vironmental data have hinted at pre-Holocene rainforest foraging, earlier human reliance on rainfores
109 sumptions by relating field abundance of the rainforest fruit fly Drosophila birchii to ecological ch
111 The thermal environments of this Panama rainforest generate a range of CTmax subsuming 74% of th
114 , followed emerging savannah corridors, with rainforest habitats repeatedly imposing temporal barrier
115 e 2 species coexist are areas where pristine rainforest has been degraded, results also suggest that
118 illus cereus biovar anthracis, in a tropical rainforest have severe consequences for local wildlife c
122 ted with the pygmy phenotype in the Batwa, a rainforest hunter-gatherer population from Uganda (east
123 he first socio-economic interactions between rainforest hunter-gatherers and farmers introduced by th
125 e confers a selective advantage for tropical rainforest hunter-gatherers but raising questions about
126 hen we expanded our analysis to include Baka rainforest hunter-gatherers from Cameroon and Gabon (wes
128 has had an impact on the genetic history of rainforest hunter-gatherers-historically referred to as
131 lia; AmazonFACE in a highly diverse, primary rainforest in Brazil; BIFoR-FACE in a 150-yr-old deciduo
132 In this study, selectively logged tropical rainforest in Indonesian Borneo is shown to contain high
134 of ecological data from a protected primary rainforest in Malaysia to illutrate how subsidies from n
138 the forests of the North American temperate rainforests in Alaska, which store >2.8 Pg C in biomass
141 nning experimental drought study in tropical rainforest (in the Brazilian Amazon), we test whether ca
144 how that the vegetation canopy of the Amazon rainforest is highly sensitive to changes in precipitati
148 The presence of a high-diversity tropical rainforest is unexpected, because other Paleocene floras
151 large majority of plant species diversity in rainforests is recent, suggesting (episodic) species tur
152 t of carbon that is being absorbed by mature rainforests is similar to or greater than that being rel
153 Old-growth forest conservation in tropical rainforests is therefore a highly-recommended solution f
154 Here, we show that some insects, such as rainforest katydids, possess equivalent biophysical mech
155 -year field study of Propithecus edwardsi, a rainforest lemur from Madagascar with a maximum lifespan
156 ithecus diadema, n = 3), endangered Malagasy rainforest lemurs, and we report extremely efficient rec
157 vorous insects in this Paleocene Neotropical rainforest may reflect an early stage in the diversifica
158 e inter-annual variability and that tropical rainforests may become less relevant drivers in the futu
162 , to our knowledge, the earliest evidence of rainforest occupation by AMH, and underscores the import
164 tion zone between the Saharan desert and the rainforests of Central Africa and the Guinean Coast, exp
165 throughout secondary succession in tropical rainforests of north-east Costa Rica, and that attempts
168 Homo sapiens' relationship with the tropical rainforests of South Asia is therefore long-standing, a
169 andscapes currently occupied by the seasonal rainforests of southern Amazonia may therefore not have
173 lution of the biomass dynamics of the Amazon rainforest over three decades using a distributed networ
181 g 17 consecutive years of data from tropical rainforest plots in Costa Rica that range from 10 y sinc
185 When populations did move from savannah into rainforest, rates of migration were slowed, delaying the
189 ining climate change feedbacks from tropical rainforests requires an understanding of how carbon gain
190 ing the ecological integrity of Kalimantan's rainforests requires immediate transnational management.
192 show that human foragers relied primarily on rainforest resources from at least ~20,000 years ago, wi
195 ng sustainability, the other in the northern rainforest-savanna mosaic, with species of greater hunti
198 na, a tree from the South American temperate rainforest shows strong heteroblasty affecting leaf shap
201 an syntypes of U. kikkawai show that it is a rainforest species occurring from Costa Rica to Brazil.
204 we suggest that the overall carbon budget of rainforests, summed across terrestrial and aquatic envir
205 thin ecosystems: across 31 trees in a Panama rainforest, surfaces exposed to sun were 8 degrees C war
207 ' are large stands of trees in the Amazonian rainforest that consist almost entirely of a single spec
208 appear to have filled a niche in Australia's rainforests that has not been occupied by any other mamm
210 a long-term drought experiment in the Amazon rainforest to evaluate the role of leaf-level water rela
211 ze the response of an old-growth Neotropical rainforest to the severe heat and drought associated wit
212 , pH, conductivity, and total alkalinity) in rainforests to those more typical for savannah systems.
213 limits of D(V) typical of modern megathermal rainforest trees first appear during a second wave of in
215 ryptic predator from the soils of the Amazon rainforest was inferred from several nuclear genes, sequ
216 ing a fertilization experiment in a tropical rainforest, we evaluated how variable substrate stoichio
217 d Bantus, living in the southern Cameroonian rainforest, were matched for sex, age, and ethnicity wit
218 behavior related to perch selection, even in rainforests where much of the solar radiation is shielde
220 d ant-seed mutualism occurs in the Amazonian rainforest, where arboreal ants collect seeds of several
221 tes are dominant species in primary tropical rainforests, where their abundance and diversity contrib
222 changes in the net carbon flux of a tropical rainforest which experiences a pronounced dry season.
223 ed to condensational latent heating over the rainforest, which strongly enhances atmospheric moisture
224 e that urban markets can defaunate deep into rainforest wilderness has implications for other urbaniz
225 l BNF within the historical area of tropical rainforest with current anthropogenic N inputs indicates
227 ear to have allowed for the establishment of rainforests within 1.4 million years of the K-T boundary
228 a prominent plant group in lowland tropical rainforests world-wide but also occur in all other tropi
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