ライフサイエンスコーパス: coral

1 e.g., number of patches) relative to healthy coral.

2 ellate and deep-water azooxanthellate fossil corals.

3 input has a positive or negative effect for corals.

4 entially aiding the adaptation of long-lived corals.

5 , including disruption of settlement cues to corals.

6 uses has emerged from metagenomic studies of corals.

7 erial communities and bacterial symbioses of corals.

8 n isotopic ratio offset identified in modern corals.

9 ration into plankton and, in turn, the atoll corals.

10 It was reported that cnidarian soft corals [21] and box jellyfish [22, 23] exhibit periods o

11 Declines in coral abundance have been linked to increased sedimentat

12 refore provides a novel system to understand coral acclimatisation to complex climatic scenarios and

13 leation of the solid mineral phase driven by coral acid-rich proteins.

14 rnis were significantly more damaging to the coral Acropora intermedia growing in the field if these

15 se pigments differ between healthy coral and coral affected by a tissue loss disease.

16 a publicly available metabolomic dataset of coral, algal, and fungal mat holobionts (i.e., the host

17 r corals, that algal allelopathy can mediate coral-algal interactions, and that OA may enhance the al

18 als (Lymphoma Academic Research Organization-CORAL and Canadian Cancer Trials Group LY.12) and 2 obse

19 ion of those pigments differ between healthy coral and coral affected by a tissue loss disease.

20 , sand beaches and dunes, seagrass beds, and coral and oyster reefs.

21 or the re-evaluation of the baseline for red coral and question the sustainability of the exploitatio

22 Both coral and Symbiodinium spp. transcriptomes from orange m

23 We show in both coral and synthetic aragonite spherulites that crystal g

24 could result from parallel responses of the coral and the microbial community to living at high natu

25 nce from the analysis of sediments and fish, coral and urchin subfossils within cores from Caribbean

26 Coral and zooxanthellae delta(15)N values were also high

27 t guano-derived nitrogen is assimilated into corals and contributes to their nitrogen requirements.

28 cosystem states, discuss traits of resilient corals and coral reef ecosystems, and propose a decision

29 The relationship between corals and dinoflagellates of the genus Symbiodinium is

30 and reproduction are strongly associated in corals and highlight benefits of delaying mutualist part

31 to enhance environmental stress tolerance of corals and the success of coral reef restoration efforts

32 environments that appear unsuitable to many corals and with increased sedimentation this acclimation

33 sile suspension feeders such as brachiopods, corals, and bryozoans to recover rapidly.

34 interactions between the tiny polyps of the coral animal in concert with its unicellular symbiotic a

35 We present a novel approach whereby young corals are 'seeded' on the reef without the need for man

36 mal susceptibility, and that central Red Sea corals are more sensitive to thermal anomalies as compar

37 variable habitats and changes over time when corals are reciprocally transplanted.

38 a change in the stress response capacity of corals as key parts of this process.

39 precedented coral loss and homogenization of coral assemblages globally, we investigate the inherent

40 no information on how water flow affects the coral-associated bacterial community under these conditi

41 revealed that there are few prior reports of coral-associated corneal toxicity and that some species

42 In particular, coral-associated viruses have received little attention,

43 old reductions in disease levels compared to corals at paired sites without adjacent seagrass meadows

44 avating sponges depended on the intensity of coral bleaching and consequent coral mortality.

45 malies caused by global warming that induced coral bleaching and mortality events globally.

46 omalous seawater temperatures and consequent coral bleaching and mortality influence these shifts.

47 ver 100 years suggested successive events of coral bleaching could shift algae-coral dominated reefs

48 The 2014-2016 global coral bleaching event has sharpened the focus on such in

49 Much of this decline is attributable to mass coral bleaching events and disease outbreaks, both of wh

50 e response of coral-excavating sponges after coral bleaching events.

51 Mass coral bleaching quickly ensued, killing 40% of the resid

52 to suffer from repeated impacts of cyclones, coral bleaching, and outbreaks of the coral-eating crown

53 eratures triggered a pan-tropical episode of coral bleaching, the third global-scale event since mass

54 Little is known about how stony corals build their calcareous skeletons.

55 ns changes the microbiome for heat-sensitive corals, but not for heat-tolerant corals growing in habi

56 Nevertheless, corals can be adapted to their thermal environment and i

57 ucture of microhabitats, driven by growth of coral colonies and contraction of skeletons, are extreme

58 scalability, the model was also run with 271 coral colonies monitored in St. Croix, US Virgin Islands

59 uantify changes in the external structure of coral colonies of tabular Acropora spp., the dominant ha

60 were employed to separate and quantify live coral colonies versus dead framework.

61 hifts from corals to excavating sponges, 217 coral colonies were monitored over 10 years (2000-2010)

62 ence that the potential to support secondary coral colonisation increases with corallith size.

63 7% of tetrapods still harboured at least one coral colony, and overall, this approach resulted in a 5

64 Consequently, observations from coral communities under naturally occurring extremes hav

65 Coral communities within the lagoon system exhibited hig

66 quickly ensued, killing 40% of the resident coral community in an event unprecedented in at least th

67 y supports the importance of the acclimatory coral condition in addition to the previous thermal hist

68 agent, environmental stressors compromising coral condition might play a larger role in disease outb

69 is hypothesised to advantage macroalgae over corals, contributing to these shifts, but the mechanisms

70 in we reviewed the phenomenon of free-living corals (coralliths), examined whether they have the capa

71 The precious Mediterranean red coral Corallium rubrum has been intensively exploited si

72 In a coral core from Dongsha Atoll, a remote coral reef ecosy

73 f-thorns starfish (COTS), losing much of its coral cover in the process.

74 omposition, and was not a simple function of coral cover on the studied reefs.

75 tand the role of reduced herbivory in recent coral declines, we produce a high-resolution 3,000 year

76 l-bound organic matter in the stony deep-sea coral Desmophyllum dianthus, a tool for reconstructing s

77 is, a mutualistic relationship scleractinian corals developed with zooxanthellae; however, because zo

78 periodicities in the records of three common coral diseases (white-band disease, yellow-band disease,

79 ttle attention, and their potential roles in coral diseases are largely unknown.

80 Yet, the temporal dynamics of coral diseases are rarely reported.

81 ad, our work suggests that the prevalence of coral diseases is dynamic and complex.

82 symbiosis, and possibly some of the numerous coral diseases that have yet to be assigned a causative

83 ena, especially the causative agents of many coral diseases.

84 eratures appear to influence the dynamics of coral diseases.

85 events of coral bleaching could shift algae-coral dominated reefs into algae-sponge dominated.

86 e critical role of parrotfish in maintaining coral-dominated reef habitat and the urgent need for res

87 ogenic stressors can cause phase shifts from coral-dominated to algal-dominated states.

88 Coral-dwelling gall crabs (Cryptochiridae) are obligate

89 lones, coral bleaching, and outbreaks of the coral-eating crown-of-thorns starfish (COTS), losing muc

90 odinium is fundamental to the functioning of coral ecosystems.

91 n) was developed to evaluate the response of coral-excavating sponges after coral bleaching events.

92 Early Miocene (18-20 Ma) corals exhibit the same nitrogen isotopic ratio offset i

93 stems ranging from the surface of threatened corals exposed to above-average temperatures, to the lun

94 ability to establish disease, while healthy corals exposed to uninhibited WBD bacterial communities

95 fragmented fluorescent pigments in diseased coral extended 3.03 mm +/- 1.80 mm adjacent to the disea

96 Our study demonstrates that coral fluorescence can be used as a proxy for coral heal

97 Do corals form their skeletons by precipitation from soluti

98 If this is how other corals form their skeletons, perhaps this is how a few c

99 In contrast, corals from the central Red Sea are close to their therm

100 rofiles in three cellular compartments: host coral gastrodermal cells, LBs, and in hospite Symbiodini

101 Lipid bodies (LBs) in the coral gastrodermal tissues are key organelles in the reg

102 -sensitive corals, but not for heat-tolerant corals growing in habitats with natural high heat extrem

103 ire individual colonies in situ, quantifying coral growth and contraction.

104 the northern GBR may already be constraining coral growth and reef resilience.

105 hed or exceeded the long-term summer maxima, coral growth during summer periods was equal to, if not

106 ence on spatiotemporal patterns of branching coral growth, and high summer temperatures in the northe

107 nd contentious) to determine whether ancient corals harbored symbionts.

108 At a sedimented reef in Indonesia (Wakatobi) corals have declined and the photoautotrophic sponge Lam

109 While reef-building corals have persisted in various forms for over 200 mill

110 For example, Late Triassic corals have symbiotic values, which tie photosymbiosis t

111 on, the diverse microbes that associate with corals have the capacity for more rapid change, potentia

112 Deterioration of coral health and associated change in the coral holobion

113 ts are widely used to forecast reef-building coral health into the future, but often fail to account

114 oral fluorescence can be used as a proxy for coral health state, and, such patterns may help refine h

115 scanning confocal microscopy to investigate coral health state.

116 pothesis is that the microbial community and coral heat tolerance are causally linked.

117 uisition is sedimentation because it impedes coral heterotrophic feeding and their ability to photosy

118 ven species of Pocillopora represented by 15 coral holobiont metagenomic libraries.

119 of coral health and associated change in the coral holobiont's bacterial community are often a result

120 antly, particular bacterial taxa predict the coral host response in a short-term heat stress experime

121 While the coral host showed significant genetic differentiation be

122 g over depth, and genetic differentiation by coral host) were examined.

123 es may co-occur and interact within a single coral host, leading to patterns of associations that can

124 In the coral host, only 61 genes were differentially expressed

125 genesis in LBs is significantly regulated by coral hosts and the lipid metabolites within holobionts

126 Montastraea cavernosa is a common coral in the Caribbean basin found in several color morp

127 Acropora spp., the dominant habitat-forming corals in shallow exposed reefs across the Pacific.

128 he 2015-2016 El Nino event during which time corals in the northern Red Sea did not bleach despite hi

129 Together, our data demonstrate that corals in the northern Red Sea have a much higher heat t

130 ovides a distinct physiological advantage to corals in the rigors of the reef, a crowded and fiercely

131 In contrast, corals in winter exhibit symbionts with higher capacity

132 example of this paradox is the reef-building corals, in which 71% of species horizontally acquire alg

133 o understand possible outcomes of the sponge-coral interaction and build the descriptive model, spong

134 Here, we show that the microbiome of reef corals is different across thermally variable habitats a

135 The use of sexually propagated corals is gaining popularity as an approach for reef res

136 The evolutionary success of reef-building corals is often attributed to photosymbiosis, a mutualis

137 Similarly, experiments suggest that coral larvae can distinguish between the water from heal

138 e results described the first settlement for coral larvae produced from cryopreserved sperm and estab

139 Therefore, the ability of coral larvae to navigate to reefs while in the open-ocea

140 ecovery by facilitating both the delivery of coral larvae to the substratum and settlement.

141 trates (7.9 and 9.8 cm in diameter) on which coral larvae were settled.

142 se a meta-analytic approach to document that coral larval swimming speeds are orders of magnitude low

143 ggest that, before intense exploitation, red coral lived in relatively high-density populations with

144 ield surveys of more than 8000 reef-building corals located adjacent to seagrass meadows showed twofo

145 At a time of unprecedented coral loss and homogenization of coral assemblages globa

146 o these shifts, but the mechanisms affecting coral-macroalgal interactions under OA are unknown.

147 Other mechanisms also affect coral-macroalgal interactions under OA, and OA further s

148 It has been suggested that reef corals may adapt to climate change by changing their dom

149 Such a mechanism suggests that stony corals may be able to sustain calcification even under l

150 g ecologically significant microbes within a corals' microbial soup.

151 tic programming, and the manipulation of the coral microbiome) as a means to enhance environmental st

152 We demonstrate that the Hawaiian coral Montipora capitata consistently emits cyan and red

153 Disease causes significant coral mortality worldwide; however, factors responsible

154 pre-empt macroalgal dominance following mass coral mortality.

155 intensity of coral bleaching and consequent coral mortality.

156 Scleractinian corals of the genus Pocillopora (Lamarck, 1816) are noto

157 te platforms produced by reef-building stony corals over geologic time are pervasive features around

158 to date demonstrating patients with aquarium coral palytoxin-associated corneal toxicity, and is the

159 corneal toxicity after exposure to aquarium coral palytoxin.

160 that lesions appeared due to changes in the coral pathobiome (multiple bacterial species associated

161 We demonstrate that the coral pathogen Vibrio coralliilyticus causes a rapidly l

162 es confirmed coral recruitment to be key for coral persistence.

163 ctivity, but also higher sensitivity to lose coral photosynthesis under heat-stress.

164 ne datasets, which are most commonly used in coral phylogenies to date, were less informative and con

165 the severity of the impact of heat-stress on coral physiology, but also the dependence of this respon

166 pic (delta(15)N) values of the scleractinian coral Pocillopora damicornis on fringing reefs around tw

167 e report the discovery of an exceptional red coral population from a previously unexplored shallow un

168 ic scenarios and may serve as a reservoir of coral populations already resistant to extreme environme

169 Disease outbreaks continue to reduce coral populations worldwide.

170 nt associated species for the persistence of coral populations.

171 It is generally assumed that stony corals precipitate calcium carbonate extracellularly as

172 Reef-building corals provide the foundation for the structural and bio

173 ral complexity at a number of scales assists coral recovery by facilitating both the delivery of cora

174 at reef structural complexity can facilitate coral recovery, but the mechanism remains unclear.

175 than 7 NTU near coral reefs would facilitate coral recruit survival under current and higher temperat

176 ojections and sensitivity analyses confirmed coral recruitment to be key for coral persistence.

177 centration and turbidity) on the survival of coral recruits of the species, Porites astreoides.

178 We found that the capacity of coral recruits to survive under warmer temperatures is l

179 damage to coral reefs in the region, and the coral reef "Bleaching Alert" alarm was not raised.

180 In a coral core from Dongsha Atoll, a remote coral reef ecosystem, we observe a decline in the (15)N/

181 Fishing pressure on coral reef ecosystems has been frequently linked to redu

182 What did coral reef ecosystems look like before human impacts bec

183 ht the risks of 2 degrees C ocean warming to coral reef ecosystems when global and local processes al

184 ates, discuss traits of resilient corals and coral reef ecosystems, and propose a decision tree for i

185 idea of inverted trophic biomass pyramids in coral reef ecosystems.

186 ping our understanding of fishing impacts in coral reef ecosystems.

187 ic values, which tie photosymbiosis to major coral reef expansion.

188 We examined the size spectra and biomass of coral reef fish communities at 38 US-affiliated Pacific

189 nterspecific cleaning mutualism critical for coral reef fish health, abundance and diversity.

190 Transport of coral reef fish larvae is driven by advection in ocean c

191 We investigated the population history of 28 coral reef fish species, close related, from the Gambier

192 y of a model species - a thermally sensitive coral reef fish, Chromis viridis (Pomacentridae) - to us

193 d between individuals, suggesting that every coral reef holobiont is a potential source of novel chem

194 The validity of the coral reef inverted trophic pyramid has been questioned,

195 re, agreeing with known genetic structure of coral reef organisms.

196 Monitoring and management plans for coral reef resilience should incorporate the growing thr

197 trate that the contribution of herbivores to coral reef resilience, via resistance to invasive algae

198 tress tolerance of corals and the success of coral reef restoration efforts.

199 the debate over whether predators influence coral reef structure and function and move us to ask not

200 for loss associated with the destruction of coral reef systems is economically, biologically, physic

201 g and manipulating large foraging areas in a coral reef with a class of dynamical decision-making mod

202 generalize these observations in four other coral reef-fish species.

203 In coral reef-fishes, the movement of larvae from planktoni

204 es to shape the distribution of seaweed on a coral reef.

205 r the structural and biological diversity of coral-reef ecosystems.

206 corals, sea anemones) are the foundation of coral-reef ecosystems.

207 os, a pesticide often inadvertently added to coral-reef waters, impaired visual-lateralization.

208 TR) coordinate the larval recruitment of the coral-reef-fish Acanthurus triostegus.

209 ide (DMS) is produced in large quantities at coral reefs and may be important in larval orientation.

210 Coral reefs are among Earth's best-studied ecosystems, y

211 Analyses of global databases showed that coral reefs are associated with more than half of the kn

212 Coral reefs are deteriorating under climate change as oc

213 Coral reefs are in decline worldwide.

214 Deep-sea scleractinian coral reefs are protected ecologically and biologically

215 pical dead zones worldwide, with >10% of all coral reefs at elevated risk for hypoxia based on local

216 n the controversial suggestion that pristine coral reefs have inverted trophic pyramids, with disprop

217 Many coral reefs have phase shifted from coral to macroalgal

218 Caribbean coral reefs have transformed into algal-dominated habita

219 g was unlikely to cause widespread damage to coral reefs in the region, and the coral reef "Bleaching

220 spectives to understand how nutrients affect coral reefs isolated from other anthropogenic stressors.

221 Coral reefs rely on inter-habitat connectivity to mainta

222 ich large predators influence the ecology of coral reefs remains an open and contentious question.

223 and OA further suppresses the resilience of coral reefs suffering blooms of macroalgae.

224 Panama and assess the risk of dead zones to coral reefs worldwide.

225 TU) above background to less than 7 NTU near coral reefs would facilitate coral recruit survival unde

226 odor" emanating from settlement sites (e.g., coral reefs), signaling the upstream location of desirab

227 interaction webs for diverse systems such as coral reefs, as well as the functional roles of dominant

228 verse case studies, including the decline of coral reefs, coastal defences from flooding, shifting fi

229 On coral reefs, methods to measure small changes in the str

230 hotspot for marine biodiversity held in its coral reefs, seagrass meadows, and mangrove forests, all

231 On coral reefs, structural complexity is typically measured

232 hough sponge abundance is increasing on some coral reefs, we lack information on how shifts from cora

233 erbivory is a critical ecological process in coral reefs, where diverse assemblages of fish maintain

234 Specifically on coral reefs, where fishers tend to overexploit species w

235 warming is essential to secure a future for coral reefs.

236 ssures, and perhaps none so precipitously as coral reefs.

237 rom some of Earth's most remote and pristine coral reefs.

238 introduce the 'hidden' small fishes found on coral reefs.

239 in the science, management and governance of coral reefs.

240 initiatives to enhance climate resilience of coral reefs.

241 d explore their potential ecological role on coral reefs.

242 cean, and the maintenance and degradation of coral reefs.

243 allow marine ecosystems from kelp forests to coral reefs.

244 Here we investigate the role of guano on corals reefs across scales by analyzing the stable nitro

245 ese initiatives, the health and abundance of corals reefs are rapidly declining and other solutions w

246 lorpyrifos, a pesticide often encountered in coral-reefs, impairs A. triostegus TH-levels, transforma

247 Enhanced coral respiration, alongside high particulate organic co

248 evidence that water flow is important for a coral's resistance to elevated seawater temperature, but

249 ptochiridae) are obligate symbionts of stony corals (Scleractinia).

250 ark species, from both Caribbean and Pacific Coral Sea water samples, whose geographical patterns of

251 t Symbiodinium and its cnidarian hosts (e.g. corals, sea anemones) are the foundation of coral-reef e

252 ed corneal toxicity and that some species of coral secrete a substance known as palytoxin, a potent v

253 ntial effects of seasonal acclimatization on coral sensitivity to heat-stress, has received limited a

254 ients revealed exposure to aquarium zoanthid corals shortly before disease onset.

255 , we observe a decline in the (15)N/(14)N of coral skeleton-bound organic matter, which signals incre

256 cles; and that they attach to the surface of coral skeletons, remain amorphous for hours, and finally

257 nsity, and calcification) of three branching coral species (Acropora muricata, Pocillopora damicornis

258 of PLTX analogues in Palythoa canariensis, a coral species collected in the Atlantic Ocean never desc

259 that structural complexity was influenced by coral species composition, and was not a simple function

260 seems likely that only a small selection of coral species have the ability to form coralliths, and t

261 of twelve common and understudied Caribbean coral species was measured for two months under crossed

262 ows for secondary reef colonization by other coral species.

263 work principles for the use of cryopreserved coral sperm for future reef restoration efforts.

264 Changes in coral-sponge interactions can alter reef accretion/erosi

265 Here we show in cell cultures of the stony coral Stylophora pistillata that calcium is concentrated

266 s and metagenomes obtained directly from the corals Stylophora pistillata, Pocillopora verrucosa, and

267 dinium, the endosymbiotic algae critical for coral survival, and more recently molecular evidence of

268 servation tool, which may help reef-building coral survive.

269 m their skeletons, perhaps this is how a few corals survived past CO2 increases, such as the Paleocen

270 y could help to explain the breakdown of the coral-Symbiodinium symbiosis, and possibly some of the n

271 Naturally diseased and laboratory infected coral systematically exhibited fragmented fluorescent pi

272 lift by measurements of elevated Pleistocene coral terraces.

273 in Fort Lauderdale, where 25% of the healthy corals that deteriorated were overtaken by excavating sp

274 The northern Red Sea harbours reef-building corals that live well below their bleaching thresholds a

275 microscopy evidence in Stylophora pistillata corals that two amorphous precursors exist, one hydrated

276 In contrast, corals that were exposed to faster water flow under labo

277 trate increasing OA advantages seaweeds over corals, that algal allelopathy can mediate coral-algal i

278 Corals thrive in a variety of environments, from low wav

279 ermally tolerant symbiont that flourishes in coral tissues after bleaching events.

280 olates acquired from a sponge, sea slug, and coral to examine the functional landscape of this enigma

281 Many coral reefs have phase shifted from coral to macroalgal dominance.

282 rtant factors in determining the capacity of corals to adapt to climate change through the establishm

283 if reducing local sedimentation will enable corals to better endure ocean warming, we quantitatively

284 eefs, we lack information on how shifts from corals to bioeroding sponges occur, and how environmenta

285 the model and determine possible shifts from corals to excavating sponges, 217 coral colonies were mo

286 tential for acclimatization or adaptation of corals to ocean acidification and even less about the mo

287 me required to introduce sexually propagated corals to reefs, and could possibly enable larger scale

288 ed winter and summer, of four Caribbean reef corals to similar light and heat-stress levels.

289 y attaching substrates with recently settled corals to the reef using binding materials is both time-

290 Exposing these corals to thermal bleaching conditions changes the micro

291 The Coral Triangle is a hotspot for marine biodiversity held

292 nt was estimated in 0.27 mg/g of lyophilized coral using UPLC-IT-TOF-MS.

293 Scleractinian corals vary in their sensitivity to these variables, sug

294 conditions, (ii) that two macroalgae damage corals via allelopathy, and (iii) that one macroalga is

295 d Vibrio spp. in the in situ experiment when corals were exposed to elevated temperature and slow wat

296 tion and build the descriptive model, sponge-corals were monitored in San Andres Island, Colombia (20

297 mon macroalgae are more damaging to a common coral when they compete under CO2 concentrations predict

298 /or spatial variation in growth of branching corals, which are important contributors to the structur

299 Corals worldwide are facing population declines due to g

300 diverse marine hosts including reef-building corals, yet their function remains unknown.

301 n a suite of modern and fossil scleractinian corals (zooxanthellate- and azooxanthellate-like) with v