ライフサイエンスコーパス: mangrove

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

2 ns from salt marshes, but not seagrasses and mangroves.

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

4 minated reef producers to isoprene-dominated mangroves.

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

6 ith it being significantly lower in lagoonal mangroves.

7 er events allowing for poleward expansion of mangroves.

8 n annually in flood protection benefits from mangroves.

9 y up to 24% in areas that are unprotected by mangroves.

10 scading impacts on connected coral reefs and mangroves.

11 lots covering undisturbed and LULCC-affected mangroves (0-, 5-, 10-, 15- and 25-year-old post-harvest

12 e); whereas, a community with more extensive mangroves (25.6 m per meter of coastline) experiences a

13 l act as net methane sources (median, range; mangrove: 279.17, -67.33 to 72,867.83; salt marsh: 224.4

14 derable declines in area, losses of lagoonal mangroves (- 6.9%) were nearly twice that of other types

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

16 and on docks within the marsh, an artificial mangrove analogue.

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

18 hes in northeast Florida has shifted between mangrove and salt marsh dominance at least 6 times betwe

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

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

21 inorg) yr(-1) and 15-62 TgC(inorg) yr(-1) in mangrove and seagrass ecosystems, respectively.

22 ium carbonates (CaCO(3)) often accumulate in mangrove and seagrass sediments.

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

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

25 ross most datasets, and tropical grasslands, mangroves and montane grasslands also have <1% of land i

26 grove carbon dynamics and the persistence of mangroves and other coastal wetlands under future scenar

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

28 ata to show that the current ecotone between mangroves and salt marshes in northeast Florida has shif

29 For example, in warmer waters, mangroves and seagrasses are in decline and benthic orga

30 ated coastal ecosystems (VCE; tidal marshes, mangroves and seagrasses) to mitigate greenhouse gas emi

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

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

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

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

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

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

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

38 While efforts to restore and protect mangroves appear to be effective over decadal timescales

39 In the tropics, mangroves are a ubiquitous component of healthy coastal

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

41 Mangroves are among the most well described and widely s

42 Mangroves are among the world's most carbon-dense ecosys

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

44 h up to 70% of ecosystem carbon is lost when mangroves are converted to shrimp ponds, some abandoned

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

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

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

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

49 a, a region that supports 10% of the world's mangrove area.

50 lutionary histories when colonising the same mangrove areas in southeastern Brazil, with other factor

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

52 These results demonstrate the value of mangroves as natural coastal defenses at global, nationa

53 Results highlight the importance of mangroves as novel systems that can rapidly accumulate C

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

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

56 ecosystems, with coral reefs, seagrasses and mangroves at most risk.

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

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

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

60 on their sedimentary setting, with carbonate mangroves being less abundant than terrigenous, represen

61 ple is fully mitigated in areas protected by mangrove belts of 1 km or more.

62 Here, we present a new global mangrove biophysical typology and show that, based on th

63 morphic setting controls natural dynamics of mangrove blue carbon stocks, while long-term land-use ch

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

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

66 nments where salt marshes, oyster reefs, and mangroves can develop and survive external stresses.

67 This paper evaluates whether mangroves can mitigate the impact of hurricanes on econo

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

69 have important implications for forecasting mangrove carbon dynamics and the persistence of mangrove

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

71 Our data suggest that mangrove carbon pools can rebuild in abandoned ponds ove

72 oil organic matter (SOM) are closely tied to mangroves' carbon sink functions and resistance to risin

73 ajority (~45%) of this increase is driven by mangrove CH(4) fluxes.

74 ocal scales, which can inform incentives for mangrove conservation and restoration in development, cl

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

76 As a result, alarming losses of mangrove, coral reef, seagrass, kelp forest and coastal

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

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

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

80 events with coastal communities experiencing mangrove deforestation are increasingly vulnerable to ec

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

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

83 ive benefits may be more cost effective, and mangrove deforestation more damaging, than previously th

84 The impact of mangrove deforestation on carbon emissions has been repo

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

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

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

88 quantify biophysical factors that determine mangrove dispersal and connectivity, including the influ

89 leaves and were more attracted to cues from mangroves distant from human settlement.

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

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

92 in southwestern (94 +/- 13 kg ha(-1) d(-1)) mangrove-dominated estuaries compared to the southeaster

93 ied SOM decay; (c) changing tidal regimes in mangroves due to sea level rise might attenuate increase

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

95 ng restoration potential and for quantifying mangrove ecosystem service provision.

96 hat polycyclic musks and MTCS are present in mangrove ecosystems and can accumulate in the tissues of

97 avior of several legacy and emerging HOCs in mangrove ecosystems in Singapore.

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

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

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

101 the behavior of legacy and emerging HOCs in mangrove ecosystems.

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

103 of ecosystem-scale CH(4) flux (F(CH4) ) from mangrove ecosystems.

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

105 the SOM decay rate, suggesting that previous mangrove elevation gain, which has allowed mangroves to

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

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

108 hanges in ecosystem services associated with mangrove encroachment.

109 Mangroves enhance fisheries and coastal protection, and

110 tes show freshwater wetlands transitioned to mangrove environments 4-3.6 ka, followed by estuarine en

111 exceeded mudflats by 434 +/- 33 Mg C/ha, and mangrove establishment increased average coastal accreti

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

113 It is uncertain whether such mangrove expansions are due to anthropogenic climate cha

114 f 5.4-6.7 mo for a community with an average mangrove extent (6.3 m per meter of coastline); whereas,

115 Meanwhile, we showed that mangrove F(CH4) could offset the negative radiative forc

116 Our results showed that daily mangrove F(CH4) reached a peak of over 0.1 g CH(4) -C m(

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

118 stocks were found in estuarine interior (EI) mangroves, followed by open coast interior, open coast f

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

134 Globally, carbon-rich mangrove forests are deforested and degraded due to land

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

136 Mangrove forests capture and store exceptionally large a

137 Mangrove forests expanded between 9800 and 7500 years ag

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

139 Mangrove forests have experienced extensive deforestatio

140 Mangrove forests have the capacity to keep pace with sea

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

142 cuss the results of conservation efforts for mangrove forests in recent years.

143 this clade, Kryptolebias ocellatus, inhabits mangrove forests in southeast Brazil; however, its matin

144 The mangrove forests of Southeast Asia are highly biodiverse

145 mangrove protection by mapping the width of mangrove forests on the path to the coast.

146 Mangrove forests play an important role in climate chang

147 Mangrove forests provide many ecosystem services but are

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

149 Sequestration potential of novel mangrove forests should be taken into account when consi

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

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

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

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

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

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

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

157 -1) ), double the global mean for old growth mangrove forests, suggesting that C accumulation from yo

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

159 rainforests and coastal defence provided by mangrove forests.

160 he net radiative cooling effect of estuarine mangrove forests.

161 esolution estimates of the economic value of mangroves forests for flood risk reduction every 20 km w

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

163 ynamics of the past 400 years for a tropical mangrove-fringed lagoon system in Java, Indonesia, Hapsa

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

165 molecular convergence, we sequenced multiple mangrove genomes.

166 ove tree crab Aratus pisonii in its historic mangrove habitat, the suboptimal colonized salt marsh ec

167 n and generate connectivity matrices between mangrove habitats using a range of floating periods.

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

169 Avicennia officinalis and other mangroves have adaptations such as ultrafiltration at th

170 f the studies assessing hurricane impacts on mangroves have focused on negative effects without consi

171 Over the past few decades, mangroves have rapidly displaced salt marshes near multi

172 and subtropical communities across 23 major mangrove-holding countries.

173 Determining the efficacy of mangroves in achieving climate goals can be complicated

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

175 To date, the benefits of mangroves in terms of protecting coastal areas have been

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

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

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

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

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

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

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

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

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

185 The mangrove killifish clade is composed of the two only kno

186 Because mangrove leaf litter is a predictable cue to coastal hab

187 coastal habitats, chemical information from mangrove leaves could provide a source of settlement cue

188 field, experimental reefs supplemented with mangrove leaves grown away from humans attracted more fi

189 o-Pacific (Fiji) were attracted to cues from mangroves leaves and were more attracted to cues from ma

190 By contrast, mangroves left to regenerate for more than 25 years reac

191 4%, equivalent to 30-60 Mg CO(2) -eq/ha over mangrove lifetime (100 year sustained global warming pot

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

193 variability could further hasten the loss of mangrove-lined coastlines, compounded by the reductions

194 0 m resolution global maps of the drivers of mangrove loss from 2000 to 2016, capturing both human-dr

195 imp aquaculture is among the major causes of mangrove loss globally.

196 Global mangrove loss has been attributed primarily to human act

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

198 ally relevant understanding of the causes of mangrove loss.

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

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

201 Mangroves may directly or indirectly influence soil accr

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

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

204 y differences in aboveground biomass between mangroves of different types, with it being significantl

205 c, process-based valuation of the effects of mangroves on averting damages to people and property.

206 aii Islands and help explain the presence of mangroves on the latitudinal outlier Bermuda.

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

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

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

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

211 ry offers an opportunity to examine the role mangroves play in climate mitigation and adaptation both

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

213 Yet, crabs in the mangrove produced the highest quality larvae.

214 ion and associated nutrient fertilization on mangrove productivity and resilience.

215 -resolving numerical ocean model to simulate mangrove propagule dispersal across the global ocean and

216 mages using a detailed wind field model, and mangrove protection by mapping the width of mangrove for

217 analyses with economic models, and find that mangroves provide flood protection benefits exceeding $U

218 Thus, although recent mangrove range expansion should indeed be placed into a

219 isplaced salt marshes near multiple poleward mangrove range limits, including in northeast Florida.

220 of abandoned ponds, associated with natural mangrove regeneration.

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

222 These results suggest that mangrove restoration efforts for protective benefits may

223 an previously thought, with implications for mangrove restoration.

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

225 elf-fertilizing hermaphroditic fish species, mangrove rivulus (Kryptolebias marmoratus), we test the

226 izes 97 studies describing CH(4) fluxes from mangrove, salt marsh, and seagrass ecosystems and discus

227 Together CH(4) emissions from mangrove, salt marsh, and seagrass ecosystems are about

228 Vegetated coastal ecosystems (VCEs; i.e., mangroves, salt marshes, and seagrasses) play a critical

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

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

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

232 macrofaunal bioturbation, namely intertidal mangrove sediment, and explored the assembly of bacteria

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

234 yclic aromatic hydrocarbons were measured in mangrove sediments, clams, and caged mussels.

235 2) storage by methane (CH(4) ) production in mangrove sediments.

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

237 Mangroves shelter coastlines during hazardous storm even

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

239 an assessment of blue carbon storage at five mangrove sites across West Papua Province, Indonesia, a

240 imp ponds, some abandoned ponds contain deep mangrove soils (>2.5 m) and large carbon reservoirs exce

241 We quantified how mangrove SOM decay is affected by predicted global warmi

242 ew studies have investigated the response of mangrove SOM dynamics to likely future environmental con

243 ill lead to a better understanding of global mangrove species distributions and their response to cha

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

245 As a result, all mangrove species showed a significant increase in litter

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

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

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

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

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

251 Ecosystem C stocks of mangrove stands exceeded mudflats by 434 +/- 33 Mg C/ha,

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

253 Undisturbed mangroves stored total ecosystem carbon stocks of 182-2,

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

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

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

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

258 n their 2016 extent, 40.5% (54,972 km(2)) of mangrove systems were deltaic, 27.5% (37,411 km(2)) were

259 28,493 km(2)) were open coast, with lagoonal mangroves the least abundant (11.0%, 14,993 km(2)).

260 In this mangrove, the mean annual CH(4) emission was 11.7 +/- 0.

261 Coastal wetlands (mangrove, tidal marsh and seagrass) sustain the highest

262 Despite low RSLR rates, the rapid mangrove to estuarine transgression was facilitated by a

263 Here, we assess the impact of mangrove to shrimp pond conversion on ecosystem carbon s

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

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

266 The response of mangroves to high rates of relative sea level rise (RSLR

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

268 s mangrove elevation gain, which has allowed mangroves to persist in areas of sea level rise, might r

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

270 t(3) and to intact ecological gradients-from mangroves to tropical alpine grasslands-that are unmatch

271 We investigated the reproduction of the mangrove tree crab Aratus pisonii in its historic mangro

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

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

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

275 Several clades of mangrove trees independently invade the interface betwee

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

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

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

279 Mangroves vary substantially according to their geomorph

280 We explore the limits of mangrove vertical accretion to sustained periods of RSLR

281 The timing of initiation and rate of mangrove vertical accretion were compared with independe

282 conservation efforts and a lack of remaining mangroves viable for conversion.

283 The generated HOC concentration data for mangrove water, sediments, and biota samples was further

284 Mangroves were also classified based on their sedimentar

285 If mangroves were lost, 15 million more people would be flo

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

287 found it very likely (>90% probability) that mangroves were unable to initiate sustained accretion wh

288 stem-scale F(CH4) in a subtropical estuarine mangrove wetland based on 3 years of eddy covariance mea

289 to characterize ecosystem-scale F(CH4) in a mangrove wetland with long-term eddy covariance measurem

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

291 Mangrove wetlands are also valuable ecosystems for promo

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

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

294 The role of coastal mangrove wetlands in sequestering atmospheric carbon dio

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

296 Mangrove wetlands provide ecosystem services for million

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

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

299 t change community structure and function of mangrove wetlands.

300 For mangroves, which are highly susceptible to climate chang

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