ライフサイエンスコーパス: mangrove

1 minated reef producers to isoprene-dominated mangroves.

2 ystems such as coral reefs, salt marshes and mangroves.

3 er events allowing for poleward expansion of mangroves.

4 n doubled when adult habitat is connected to mangroves.

5 with 1.5-7.2 mm yr(-1) for nearby reference mangroves.

6 onfidence interval (C.I.)] for BGC in Kenyan mangroves.

7 magery, we linked FDD to observed changes in mangrove abundance in Florida, further exemplifying the

8 Intertidal wetlands, primarily salt marsh, mangrove and mudflats, which provide many essential ecos

9 amined how biotic interactions between black mangrove and salt marsh vegetation along the Texas coast

10 nature of biotic interactions between black mangrove and salt marsh vegetation: (i) Salt marsh veget

11 Sediment OC stocks did not differ between mangrove and saltmarsh habitats.

12 hest in flooded grasslands (1.26 km yr(-1)), mangroves and deserts.

13 s showed differential expression between the mangroves and glycophytes, reminiscent of the adaptive s

14 We estimate that mangroves and halophyte scrubs in Mexico's arid northwes

15 us guacamaia, has a functional dependency on mangroves and has suffered local extinction after mangro

16 lture and tourism developments that threaten mangroves and result in costly "externalities." Specific

17 To compare how well mangroves and salt marshes accommodate sea-level rise, w

18 ore effective conservation of the Sundarbans mangroves and the many other species that rely on them.

19 Given their relatively small area, mangroves and their organic sediments are of disproporti

20 erstanding of sediment elevation dynamics in mangroves and tidal marshes has been gained by monitorin

21 ommon with the other 'blue carbon' habitats (mangroves and tidal marshes) seagrasses are thought to p

22 positively related to the local abundance of mangroves and, in particular, to the productive area in

23 oth cordgrass) or Avicennia germinans (black mangrove) and in mixed stands containing both species.

24 s that quantify services provided by corals, mangroves, and seagrasses.

25 reases herbivory in salt marshes, but not in mangroves, and that this effect increases with increasin

26 Modern mangroves are among the most carbon-rich biomes on Earth

27 Mangroves are among the most threatened and rapidly disa

28 Mangroves are among the most well described and widely s

29 The extent, productivity and preservation of mangroves are controlled by the interplay of tectonics,

30 Mangroves are disappearing rapidly worldwide despite the

31 At climatic boundaries where mangroves are expanding and replacing salt marsh, wetlan

32 covering only approximately 138 000 km(2) , mangroves are globally important carbon sinks with carbo

33 arvesting the shrimp and fish that thrive if mangroves are not cut.

34 oach are discussed, and the implications for mangroves are outlined.

35 Here we show that mangroves are unexpectedly important, serving as an inte

36 ffects of sea level rise on salt marshes and mangroves are well studied, we focus on its effects on c

37 ence of different risk factors in particular mangrove areas used in an additive manner to create a re

38 Thus, these salt marsh and mangrove assemblages were accreting sediment and buildin

39 Their close resemblance to Recent mangrove-associated copepods highlights the antiquity of

40 Gulf of Mexico coast, USA, subtropical black mangrove (Avicennia germinans) at the northern limit of

41 the global economic potential for protecting mangroves based exclusively on their carbon.

42 years of monitoring of a mangrove forest in Mangrove Bay in north Western Australia, we documented t

43 Diebacks in Mangrove Bay were coincident with periods of very low se

44 The impact of these processes on mangrove-bearing successions in the Oligo-Miocene of the

45 ificantly correlated with the actual loss of mangroves between 2000 and 2010 and the categorical risk

46 Here, we present the sRNA transcriptomes of mangroves Bruguiera gymnorrhiza and Kandelia candel.

47 Juvenile coral reef fish often inhabit mangroves, but the importance of these nurseries to reef

48 six mangrove lineages; TE load reduction in mangroves can be attributed to the paucity of young elem

49 y interact with plant processes to influence mangrove capacity to keep pace with rising sea level.

50 tes of mangrove sediment carbon stocks; most mangrove carbon is stored belowground.

51 for highlighting and prioritizing areas for mangrove conservation and restoration.

52 iencing uncontrolled cutting to one in which mangrove conservation is providing gains in income for t

53 d expansion, deforestation, overfishing, and mangrove conversion), quantitatively connecting costs bo

54 hat the majority of potential emissions from mangroves could be avoided at less than $10 per ton of C

55 Future warming may result in increases in mangrove cover beyond current latitudinal limits of mang

56 Remote sensing data of mangrove cover over time are integrated with georeferenc

57 average, we find that a 10% increase in the mangrove cover within SANAPA boundaries in a 5-km(2) rad

58 n estuary and during a 40 h time series in a mangrove creek (ecosystem scale).

59 to other samples taken from the other known mangrove data, a tropical rainforest, and ocean sediment

60 Current rates of mangrove deforestation are likely to have severe deleter

61 ate drivers (i.e., replacement land uses) of mangrove deforestation in Southeast Asia between 2000 an

62 Our study highlights frontiers of mangrove deforestation in the border states of Myanmar,

63 ue to the more complex quantitative model of mangrove deforestation.

64 hthonous scavenged skeleton was preserved in mangrove deposits, raising the possibility that titanosa

65 hydrogen isotope ratios from microalgal and mangrove-derived sedimentary lipids in the Galapagos to

66 d tidal range and bed shear stress optimized mangrove development along tide-influenced tropical coas

67 When applied to a 1992 mangrove distribution map, the BGC estimate was 75.65 Mt

68 Malayan coast, a hotspot with a large global mangrove distribution.

69 f DOC, Hg, and MeHg to coastal waters from a mangrove-dominated estuary in Everglades National Park (

70 The Sundarbans, the largest mangrove ecosystem in the world, is under threat from hi

71 tion on income components directly linked to mangrove ecosystem services.

72 he mosaic of microhabitats that constitute a mangrove ecosystem.

73 To persist, mangrove ecosystems must adjust to rising sea level by b

74 e four coral reef types (but not seagrass or mangrove ecosystems).

75 l environments was investigated in Sundarban mangrove ecosystems, Bengal Delta, Bangladesh.

76 ypes of coral reefs, as well as seagrass and mangrove ecosystems, throughout the Northern Antilles.

77 l increasing and under-recognized threats to mangrove ecosystems.

78 we provide a general overview of research on mangrove elevation dynamics, emphasizing the role of the

79 ere is quantitative evidence to suggest that mangrove encroachment may enhance carbon storage and the

80 tem structure and function, we theorize that mangrove encroachment may increase nutrient storage and

81 hanges in ecosystem services associated with mangrove encroachment.

82 Mangroves enhance fisheries and coastal protection, and

83 nalyses and target predictions revealed that mangroves exhibit distinct sRNA regulatory networks that

84 red species of Darwin's finches, such as the mangrove finch (Camarhynchus heliobates) [3].

85 nced an immediate loss in the consumption of mangrove firewood, with the loss most prevalent in riche

86 urces, this finding suggests that protecting mangroves for their carbon is an economically viable pro

87 rved winter temperature data (1970-2000) and mangrove forest and salt marsh habitat data.

88 lenge in evaluating the carbon benefits from mangrove forest conservation is the lack of rigorous spa

89 he ecological implications of these marsh-to-mangrove forest conversions are poorly understood, but w

90 imple winter climate-based models to predict mangrove forest distribution and relative abundance usin

91 of winter climate change upon salt marsh and mangrove forest foundation species in the southeastern U

92 During 16 years of monitoring of a mangrove forest in Mangrove Bay in north Western Austral

93 ify winter climate thresholds for salt marsh-mangrove forest interactions and highlight coastal areas

94 nd functional change in the form of poleward mangrove forest migration and salt marsh displacement.

95 We identified herbivory patterns in a dwarf mangrove forest on the archipelago of Twin Cays, Belize.

96 itermes corniger (Isoptera: Termitidae) in a mangrove forest on the Atlantic coast of Panama showed a

97 alt marshes to winter climate change-induced mangrove forest range expansion; and (3) What is the pot

98 ing by a wood-boring beetle in a neotropical mangrove forest system.

99 on of the microbial communities from a large mangrove forest that stretches across southwestern India

100 To implement policies that conserve mangrove forests across Southeast Asia, it is essential

101 from forests, including those from disparate mangrove forests and the tropical rain forest, from the

102 Intertidal ecosystems, including mangrove forests are among those ecosystems that are hig

103 Mangrove forests are one of the world's most threatened

104 based on our field data, which suggests that mangrove forests at sites with low tidal range and low s

105 lite imagery to demonstrate that the area of mangrove forests has doubled at the northern end of thei

106 Mangrove forests have experienced extensive deforestatio

107 Mangrove forests have the capacity to keep pace with sea

108 n of ENSO will have negative effects on some mangrove forests in parts of the Indo-Pacific that will

109 The mangrove forests of Southeast Asia are highly biodiverse

110 er climate and the presence and abundance of mangrove forests relative to salt marshes; (2) How vulne

111 e find that sediment availability can enable mangrove forests to maintain rates of soil-surface eleva

112 uture distribution and relative abundance of mangrove forests under alternative winter climate change

113 Mangrove forests were lost at an average rate of 0.18% p

114 Well-planned coastal development near mangrove forests will be essential to avert this crisis.

115 ld in its coral reefs, seagrass meadows, and mangrove forests, all of which are in global decline.

116 ra foci are located near estuaries, lagoons, mangrove forests, and on islands.

117 ndo-Pacific region holds most of the world's mangrove forests, but sediment delivery in this region i

118 e cover beyond current latitudinal limits of mangrove forests, thereby altering the structure and fun

119 rainforests and coastal defence provided by mangrove forests.

120 tween two extractive ecosystem services from mangrove forests: cutting mangroves (fuelwood) and harve

121 ol poleward range limits of three species of mangroves found in North America.

122 these fisheries is US $37,500 per hectare of mangrove fringe, falling within the higher end of values

123 stem services from mangrove forests: cutting mangroves (fuelwood) and harvesting the shrimp and fish

124 In conclusion, mangrove genomes employ a convergent strategy of TE load

125 molecular convergence, we sequenced multiple mangrove genomes.

126 s switched from negative to neutral as black mangroves grew from seedlings into juvenile trees.

127 anzania, where enforcement of prohibition of mangrove harvesting was strengthened to preserve biodive

128 The destruction of mangroves has a strong economic impact on local fishing

129 Salt marsh and mangrove have been recognized as being among the most va

130 In this study we show that mangroves in desert inlets in the coasts of the Baja Cal

131 n in estimating coastal protection values of mangroves in Thailand, we show that the optimal land use

132 Mangroves in the Caribbean strongly influence the commun

133 g coincident with the large-scale dieback of mangroves in the Gulf of Carpentaria in northern Austral

134 hat found under some of the tallest tropical mangroves in the Mexican Pacific coast.

135 ific knowledge on the spatial ecology of the mangroves in this world heritage ecosystem has been a ma

136 of mercury (Hg) and methylmercury (MeHg) in mangroves, in conjunction with the common co-occurrence

137 ence of global shifts in the distribution of mangroves, including encroachment into salt marshes.

138 ee winters have led to an expansion of black mangrove into salt marshes.

139 As phenotypic convergence among mangroves is common, the possibility of convergent adapt

140 results indicate that the expansion of black mangroves is mediated by complex biotic interactions.

141 Deforestation of mangroves is of global concern given their importance fo

142 vegetation (e.g., kelp, seagrass, marsh, and mangroves) it has been well demonstrated that alteration

143 ical drivers of growth of adult and juvenile mangrove jack (Lutjanus argentimaculatus) from tropical

144 The mangrove killifish (Kryptolebias marmoratus) is the only

145 e reduction happens independently in all six mangrove lineages; TE load reduction in mangroves can be

146 9 km) of the projected carbon emissions from mangrove loss and the cost of avoiding the emissions.

147 neralized least squares regression and using mangrove loss data from 1992 to 2000.

148 y irreparable damage to fisheries because of mangrove loss has been belittled and is greatly underest

149 Here, we identified key drivers of mangrove loss in Kenya and compared two different approa

150 The country-level mangrove map provides a valuable tool for assessing carb

151 We found that all lineages of mangroves massively and convergently reduce TE loads in

152 Mangroves may directly or indirectly influence soil accr

153 We summarize the primary ways in which mangroves may influence sediment accretion and vertical

154 Our valuation of the services provided by mangroves may prove useful in making appropriate decisio

155 Indeed, mangroves might be expected to have negligible influence

156 t of tectonic and oceanographic processes on mangrove OC sequestration within the global carbon cycle

157 half of the plots was subjected to freezing (mangrove) or wrack burial (salt marsh), which caused sho

158 Preservation of mangrove organic carbon (OC) was promoted by high tecton

159 mangrove seedlings at lower latitudes; (ii) mangroves performed well at intermediate elevations, but

160 The greatest threats to mangrove persistence are deforestation and other anthrop

161 ted from the twigs and leaves of the Chinese mangrove plant Xylocarpus granatum, together with four r

162 s used to generate a map of losses of Kenyan mangroves predicted to have occurred between 2000 and 20

163 istribution models, FDD accurately predicted mangrove presence/absence.

164 c framework to identify the causal effect of mangrove protection on income components directly linked

165 ns in shrimping and fishing that result from mangrove protection.

166 Mangrove-related fish and crab species account for 32% o

167 oves and has suffered local extinction after mangrove removal.

168 elevation (sediment accretion, subsidence), mangrove replacement of salt marsh, with or without dist

169 ributions of DOC, tidally driven export from mangroves represents a significant potential source of H

170 ts ranging from 239 to 25,198 loci) from red mangroves (Rhizophora mangle) in Florida to evaluate how

171 Among vertebrate animals, only the mangrove rivulus (Kryptolebias marmoratus) was known to

172 us genotypes in Floridian populations of the Mangrove Rivulus (Kryptolebias marmoratus).

173 wave attenuation data from field studies of mangroves, salt marshes, seagrass beds, nearshore coral

174 ne and coastal wetlands, such as marshes and mangroves, sand beaches and dunes, seagrass beds, and co

175 fforts should protect connected corridors of mangroves, seagrass beds and coral reefs.

176 of rigorous spatially resolved estimates of mangrove sediment carbon stocks; most mangrove carbon is

177 dy, we categorize the microbial community in mangrove sediment samples from four different locations

178 The depth-age curve for the mangrove sediments of Baja California indicates that sea

179 tude distribution limit, but inhibited black mangrove seedlings at lower latitudes; (ii) mangroves pe

180 (i) Salt marsh vegetation facilitated black mangrove seedlings at their high-latitude distribution l

181 (iii) different life history stages of black mangroves (seedlings vs. juvenile trees).

182 lues previously calculated worldwide for all mangrove services together.

183 The encroachment of woody mangrove shrubs and trees into herbaceous salt marshes m

184 Whole-genome sequencing of three mangrove species further shows the decline in Ne to be s

185 Significantly, less genetically diverse mangrove species suffered much greater destruction.

186 The results revealed that mangrove species was the most reliable predictor of BGC;

187 red at depths beyond 1 m, and the effects of mangrove species, location and environmental context on

188 ial density maps for the four most prominent mangrove species--Heritiera fomes, Excoecaria agallocha,

189 Conserved and mangrove-specific miRNA targets were predicted; the latt

190 of other ecological and economic functions, mangroves store considerable carbon.

191 on their own accumulated peat, these desert mangroves store large amounts of carbon in their sedimen

192 thesis of the marginolactone azalomycin F in mangrove Streptomyces sp. 211726 has shown that only nin

193 ient homeostasis as possible contributors to mangrove success in stressful environments.

194 Here we analyse recent trends in mangrove surface elevation changes across the Indo-Pacif

195 flux of dissolved organic carbon (DOC) from mangrove swamps accounts for 10% of the global terrestri

196 Although Hg and MeHg yields from tidal mangrove swamps have not been previously measured, our e

197 the effect of salt marsh vegetation on black mangroves switched from negative to neutral as black man

198 from four different locations within a vast mangrove system in Kerala, India.

199 n and pCO(2) in estuarine waterways and in a mangrove tidal creek, implying that submarine groundwate

200 Peat deposition and preservation allows some mangroves to accrete vertically and keep pace with sea-l

201 The proportional conversion of mangroves to different land use types has not been syste

202 in Myanmar, and the sustained conversion of mangroves to oil palm plantations in Malaysia and Indone

203 y, southern China, to test the robustness of mangroves to sea level changes in relation to their gene

204 dation or thermal refuge, by the herbivorous mangrove tree crab Aratus pisonii.

205 Tropical communities, anchored by mangrove trees and having experienced frequent past sea

206 events resulted in the death of half of the mangrove trees in this area.

207 Several clades of mangrove trees independently invade the interface betwee

208 gree of connection between the prop roots of mangrove trees.

209 natural product isolated from the Caribbean mangrove tunicate Ecteinascidia turbinata.

210 e interactions of the microorganism with its mangrove tunicate host.

211 h themes such as archaea, bacteria, viruses, mangroves, turtles, and ocean acidification; (3) physica

212 in particular, to the productive area in the mangrove-water fringe that is used as nursery and/or fee

213 ure trajectory of the area from one in which mangroves were experiencing uncontrolled cutting to one

214 In total, more than 100,000 ha of mangroves were removed during the study period, with aqu

215 However, loss of mangrove wetlands and these ecosystem services are a glo

216 Mangrove wetlands are also valuable ecosystems for promo

217 n, prompting the restoration and creation of mangrove wetlands as a potential solution.

218 e and potential loss of stored C for created mangrove wetlands before 2100.

219 ation change, and its components, in created mangrove wetlands over a 25 year developmental gradient.

220 Mangrove wetlands provide ecosystem services for million

221 While mangrove wetlands store C persistently in roots/soils, s

222 All created mangrove wetlands were exceeding current relative sea-le

223 nd biodiverse coral reefs, seagrass beds and mangroves, which house primary producers that are amongs