ライフサイエンスコーパス: coral

1 streoides, a disease-resistant reef-building coral.

2 tments, and over half were found uniquely in coral.

3 research on the early life-history stages of corals.

4 filter-feeding organisms such as cold-water corals.

5 ts of gene function in both larval and adult corals.

6 ew window into the dynamics of reef-building corals.

7 tress) plays an important protective role in corals.

8 xample, engineering more thermally resistant corals.

9 genomic data and genetic tools available for corals.

10 to shed light on disease pathophysiology in corals.

11 means of biopreservating and biobanking soft corals.

12 owth and physical complexity of reef-forming corals.

13 the North Atlantic by 2100 for scleractinian corals (30%-42% of present-day suitable habitat), even s

14 and database for the most speciose genus of coral, Acropora, and their symbionts.

15 ity with host age, possibly a consequence of corals adapting to degraded environments.

16 Our results indicate no clear link between coral age and microbial diversity or richness.

17 model habitat suitability for key cold-water coral and commercially important deep-sea fish species u

18 ferentially associated with turf algae, hard coral and, to a lesser extent, fleshy macroalgae microha

19 28%-100% in suitable habitat for cold-water corals and a shift in suitable habitat for deep-sea fish

20 ey often overlook other species that live on corals and influence coral-microbe interactions.

21 Aquarickettsia' within disease-susceptible corals and led to an increase in bacterial community dis

22 n approach that is particularly relevant for corals and other sessile organisms that must endure incr

23 mpass diverse symbionts that are critical to corals and other species living in coral reefs.

24 ir microbiomes has been well-established for corals and sponges, their functional roles are less well

25 Reef-building corals and their aragonite (CaCO(3)) skeletons support e

26 faveolata, a disease-sensitive reef-building coral, and Porites astreoides, a disease-resistant reef-

27 he relative condition of reefs based on live coral, and to identify potential coral refugia in the fa

28 e interactions between PAC and scleractinian corals, and elucidate the role of PAC and their associat

29 s, including the tubeworm Hydroides elegans, corals, and the hydrozoan Hydractinia, we have begun to

30 Other long-lived, sessile organisms such as corals appear to be poorly equipped to survive rapid cha

31 Scleractinian "stony" corals are major habitat engineers, whose skeletons form

32 All modern scleractinian corals are thought to produce skeletons exclusively of t

33 s that depend on live coral, suggesting that coral area could be used to predict the sensitivity of a

34 ffect of thermal stress within a subtropical coral assemblage.

35 how shifts in the morphological structure of coral assemblages affect the abundance of juvenile and a

36 ive abundance of morphological groups within coral assemblages are likely to affect population replen

37 Subtropical coral assemblages are threatened by similar extreme ther

38 d are consistent with algal exudates feeding coral-associated microbes.

39 he algal symbiont community can lead to some corals becoming more or less thermally tolerant.

40 Then, we show how coral biodiversity metrics (species richness, total abun

41 how understanding the biological control of coral biomineralization is critical to informing future

42 Most corals bleach and suffer mortality at just 1-2 degrees C

43 d on bleaching phenomena to understand where corals bleach, when and why-resulting in a large-yet sti

44 ened by environmental stressors that lead to coral bleaching (that is, the disruption of endosymbiosi

45 Despite linkage between coral bleaching and disease, the roles of symbiotic bact

46 more in the region were decimated by massive coral bleaching and mortality.

47 Using island-wide surveys of coral bleaching and nitrogen availability within a Bayes

48 t both to an extreme heatwave that triggered coral bleaching and to invasive rats which disrupt nutri

49 o turbidity, between 0.080 and 0.127 reduced coral bleaching during thermal-stress events.

50 cted in Kane'ohe Bay Hawai'i during the 2015 coral bleaching event.

51 depths, which were coincidental with a mass coral bleaching event.

52 pected increase in frequency and severity of coral bleaching events is likely to make even rapid reco

53 nteracts with temperature anomalies to alter coral bleaching for the two dominant genera of branching

54 Coral bleaching is one of the main drivers of reef degra

55 we can implement new capacity to resolve how coral bleaching patterns emerge from complex biological-

56 ider how the past three decades of intensive coral bleaching research has established the basis for c

57 Coral bleaching, caused by the loss of brownish-colored

58 s in temperature-sensitive ecosystems (e.g., coral bleaching, hypoxia) and is expected to have expand

59 agnitude of temperature anomalies that cause coral bleaching, leading to widespread mortality of ston

60 We analyzed coral bleaching, temperature, and turbidity data from 3,

61 udies have explored conditions that moderate coral bleaching.

62 by the warming oceans may extend far beyond coral bleaching.

63 out 10 m(2) and the length of the individual coral branches range from 12 to 30 cm.

64 , restoration, and research of reef-building corals but also as a laboratory for the implementation o

65 acid concentrations inferred to occur at the coral calcification site.

66 Large, intact corals can help build past (century-scale) climatic prof

67 Here, we develop 3D printed bionic corals capable of growing microalgae with high spatial c

68 The first X-ray crystal structure of a coral caspase, of PaCasp7a determined at 1.57 angstrom r

69 The algae live inside coral cells in a specialized membrane compartment known

70 as well as in the immune modulation of host coral cells.

71 s feedback makes the ecosystem more prone to coral collapse under fishing pressure but also more pron

72 the equatorial Pacific, we track individual coral colonies at sites spanning a gradient of local ant

73 ination for fluorescence microscopy of small coral colonies.

74 ion, respectively, on the decline of coastal coral communities following the development of the Pearl

75 ient pollution may enhance the resilience of coral communities in the face of mounting stresses from

76 dramatic decline of the Pearl River estuary coral communities reported from 1980 to 2000.

77 nderstand coral persistence, particularly as coral communities worldwide are declining at rapid rates

78 tress within marine systems have focussed on coral communities, and less is known about measuring str

79 These findings will help prioritize coral conservation efforts and plan assisted gene flow i

80 Changes in coral convexity, rather than live coral cover or reef ru

81 Here, we used coral cores collected in Miri-Sibuti Coral Reefs Nationa

82 al, and significantly correlates with actual coral cover changes observed throughout the region betwe

83 Between 2016 and 2019, hard coral cover did not change on deep reefs which remained

84 for adaptation and, in our model, maintained coral cover even under a rapid "business-as-usual" warmi

85 e find that during the period 1970-2014, ETP coral cover exhibited temporary reductions following maj

86 Using a 44 year dataset (1970-2014) of live coral cover from the ETP, we assess whether ETP reefs ex

87 Changes in coral convexity, rather than live coral cover or reef rugosity, disproportionately affecte

88 we surveyed C. abbreviata abundance, percent coral cover, and the abundance of potential snail predat

89 sistent with a large literature, with higher coral cover, more species of fish, and greater fish biom

90 m functions and services at reefs varying in coral cover.

91 services, on 328 Caribbean reefs varying in coral cover.

92 pite comparable benthic composition and live coral cover.

93 many the range of outcomes is not related to coral cover.

94 colonial bush or a larger bioconstruction of coral covering the sea bottom), formed entirely by the s

95 mino acids of massive, tropical Porites spp. corals cultured over different seawater pCO(2).

96 on of endosymbiosis), which in turn leads to coral death and the degradation of marine ecosystems(2).

97 ove the photophysical characteristics of the coral-derived fluorescent protein TagRFP-T.

98 uous oxygen microelectrode recordings in the coral diffusive boundary layer revealed hyperoxia during

99 Aquarickettsia' species increase coral disease risk through two mechanisms: (i) the creat

100 e been combined as a novel approach to study coral disease.

101 we investigate the ecological drivers of two coral diseases-growth anomalies and tissue loss-affectin

102 ottom), formed entirely by the scleractinian coral Eguchipsammia fistula (Alcock, 1902) (Dendrophylli

103 commodate live organisms of the size of most coral embryos (> 250 um), and sample processing is often

104 y sort live and preserved Montipora capitata coral embryos and larvae.

105 and discuss the present understanding of how corals evolved and how their skeletons changed over geol

106 Corals exemplify this concept, where shifts in the algal

107 This shows corals exhibiting a similar dynamic survival response as

108 It is currently unknown why such large corals exist around this particular island.

109 crises, with sea anemones and proteinaceous corals filling empty niches as tropical reef builders we

110 trient stoichiometry and stable isotopes per coral fragment, we found that nutrients from fish positi

111 This paper reports a deep-water coral framework (a single colonial bush or a larger bioc

112 ing or executing bleaching, or in protecting corals from it, we used RNAseq to analyze gene-expressio

113 Here, we used absolutely dated fossil corals from the central tropical Pacific to gauge ENSO's

114 of the expected higher thermal tolerance in corals from the protected reef site, denoted by an incre

115 ains crust-like resupinate fungi, polypores, coral fungi, and gasteroid forms (e.g., puffballs and st

116 changes befalling coral reefs, understanding coral gene function is essential to advance reef conserv

117 orks to improve our fundamental knowledge of coral gene function.

118 At the end of the experiment, seven of eight coral genets mainly hosted Cladocopium symbionts, wherea

119 Specifically, four 'best performer' coral genets were analyzed at the end of the experiment

120 istant and -susceptible Acropora cervicornis coral genotypes (hereafter referred to simply as 'genoty

121 across six discrete recruitment cohorts for coral grouper (Plectropomus maculatus) on the Great Barr

122 that nutrients from fish positively affected coral growth, and moderate doses of anthropogenic nutrie

123 e analysis of photogrammetric data show that coral habitats vary considerably within the upper canyon

124 despite initially resisting bleaching, these corals had no survival advantage in one species and 3.3

125 ry museum collections, and cored into modern coral heads.

126 lliophila abbreviata, are one such threat to coral health and recovery worldwide, but current underst

127 l, dispersant, oil + dispersant combined) on coral health.

128 For example, coral holobionts losing the competition with turf algae

129 escribe and predict metabolic functioning of coral holobionts, and how this functioning is regulated

130 tablished techniques to accurately determine coral host age by quantifying annual skeletal banding pa

131 res the photosynthetically fixed carbon with coral host cells while host cells provide inorganic carb

132 sal phyla, including Cnidaria (sea anemones, corals, hydras, and jellyfish), Porifera (sponges), and

133 des familiar animals including sea anemones, corals, hydroids, and jellyfish.

134 In contrast, corals in highly disturbed areas were already dominated

135 sta textilis previously reported overgrowing corals in Jamaica.

136 ing for the two dominant genera of branching corals in Moorea, French Polynesia.

137 These corals initially had heat-sensitive algal symbiont commu

138 Coral-inspired light management systems could overcome t

139 Coral is the life-form that underpins the habitat of mos

140 bionts from the host tissue of reef-building corals, is a major threat to reef survival.

141 th round corners, feathery and fibrous, or a coral-like and thread-like structure.

142 nterisland and intraisland variation in live coral location improves our understanding of reef geogra

143 habitat were projected for the scleractinian coral Lophelia pertusa and the octocoral Paragorgia arbo

144 Many studies examine coral loss and its causes-and often presume a universal

145 Especially devastating periods of coral loss frequently occur during El Nino-Southern Osci

146 Dramatic coral loss has significantly altered many Caribbean reef

147 universal decline of ecosystem services with coral loss-rather than evaluating the range of possible

148 facilitate conservation efforts to mitigate coral loss.

149 itical functional group, independent of live coral loss.

150 While growing, coral maintained homeostasis in their nutrient pools, sh

151 Hard, or stony, corals make rocks that can, on geological time scales, l

152 ulations to model adaptation to warming in a coral metapopulation comprising 680 reefs and representi

153 er species that live on corals and influence coral-microbe interactions.

154 earchers now recognize the importance of the coral microbiome, but they often overlook other species

155 ated the population genetic structure of the coral Montastraea cavernosa across eight reef sites surr

156 Considering the disparity of coral morphological growth forms in shelter provision fo

157 Nonetheless, quantifying coral morphological traits may contribute to forecasting

158 s from six species spanning all reef-forming coral morphologies: Branching, encrusting, massive, and

159 s showing higher vulnerability to changes in coral morphology.

160 Particularly catastrophic bleaching-induced coral mortality events in the past 5 years have catalyze

161 Furthermore, we demonstrate that corals of a similar age from the same reef can show very

162 ing the settlement location of scleractinian corals on tropical reefs.

163 s, indicating greater thermal sensitivity in corals once the optimum temperature is exceeded.

164 saturated calcifying fluid known to exist in corals, or from a dense liquid precursor, observed in sy

165 a Pleistocene fossil invertebrate, the stony coral Orbicella annularis.

166 ord that enables paleontological analysis of coral origins, tracing them back to the Triassic (~241 M

167 king to cultivate P. acuta, and likely other corals, over long-term timescales.

168 hed and unbleached colonies of the branching coral P. compressa collected in Kane'ohe Bay Hawai'i dur

169 le) climatic profiles, and better understand coral persistence, particularly as coral communities wor

170 habitat compartments - sediment, water, and coral (Pocillopora grandis, Montipora aequituberculata,

171 ds to alternative stable ecosystem states of coral population persistence or collapse (and complete a

172 Similarly, the viability of many tropical coral populations at higher latitudes is highly dependen

173 Combined, our results demonstrate how coral populations can persist in high pCO(2) environment

174 As coral populations decline across the Caribbean, it is be

175 ts in population growth rates (lambda) among coral populations during both stress and non-stress peri

176 to boost the adaptive potential of specific coral populations.

177 e the microbiome of the common reef-building coral, Porites lutea.

178 the extent to which bottom-up forces (i.e., coral prey), top-down forces (i.e., predators), and mari

179 l samples for effective sequencing of fossil coral proteins, allowing comparison of modern and fossil

180 Subsequently, the coral record shows that the implementation of improved w

181 Our results suggest that coral records from northern Borneo are invaluable archiv

182 e we use precisely dated and highly resolved coral records from the eastern equatorial Indian Ocean,

183 lting in a commensurate 3-5-fold increase in coral recruitment and reef fish community abundance and

184 Documenting post-bleaching trajectories of coral reef communities is crucial to understand their re

185 ng might be used to develop solutions to the coral reef crisis by, for example, engineering more ther

186 s important for guiding fishery responses to coral reef degradation.

187 highly diverse, yet increasingly threatened, coral reef ecosystem.

188 Coral reef ecosystems are among the first to fundamental

189 lture, and the recruitment of new animals to coral reef ecosystems, little is known about the mechani

190 sis-which is critical for the maintenance of coral reef ecosystems-is increasingly threatened by envi

191 ogenic change affecting Borneo's coastal and coral reef environments are lacking.

192 was the likely trigger of mass mortality of coral reef fishes in the Red Sea.

193 munity-wide gut content analyses of tropical coral reef fishes worldwide, resulting in diet informati

194 Coral reef habitats surrounding Cuba include relatively

195 orthern Mozambique Channel and should inform coral reef management decisions in the region.

196 and (b) acquisition of thermotolerance among coral reef organisms.

197 ness of their grazing on seaweed removal and coral reef recovery in two experiments conducted sequent

198 lutionary projections may better account for coral reef response to the chronic stress regimes charac

199 how they promote macroalgal dominance at the coral reef scale.

200 he network of the world's public aquaria and coral reef scientists.

201 nd population admixture of dispersal limited coral reef species, potentially impacting the ecology an

202 on effectiveness of MPAs for five species of coral reef-associated sharks (Triaenodon obesus, Carchar

203 covered that the world's officially recorded coral reef-based managed areas (with a median width of 9

204 The complexity of coral-reef ecosystems makes it challenging to predict th

205 (39)PAHs) in the livers and muscles of three coral-reef fish (50 specimens) from the Persian Gulf, Kh

206 or understanding the microbiology of healthy coral reefs and their surrounding seawater.

207 Many Caribbean coral reefs are heavily degraded, yet their pre-human, n

208 Coral reefs are on a steep trajectory of decline, with n

209 Forests and coral reefs are structurally complex ecosystems threaten

210 The numerous ecosystem services derived from coral reefs are underpinned by the growth and physical c

211 es can reverse the ecological phase shift on coral reefs away from seaweed dominance.

212 of extreme R(onset), calamities inflicted on coral reefs by the warming oceans may extend far beyond

213 several possibilities into which present-day coral reefs can transition.

214 Regions that had a greater relative area of coral reefs had higher catches of species that depend on

215 This suggests that ETP coral reefs have adapted to thermal extremes to date, an

216 termine how fisheries catches associate with coral reefs in Queensland, Australia.

217 With the persistence of Caribbean coral reefs in the balance, our findings demonstrate tha

218 arine reserves still have important roles on coral reefs in the face of climate change, the species a

219 es between the world's hottest, most extreme coral reefs in the southern Arabian Gulf and the nearby,

220 Maintaining coral reefs into the future requires not only the surviv

221 so assessing the dependency of fisheries on coral reefs is important for guiding fishery responses t

222 ciated fishes to major disturbance events on coral reefs is negative (e.g., reduced abundance and con

223 ovide an exemplar of how biotic networks and coral reefs may be impacted by anthropogenic activities.

224 we used coral cores collected in Miri-Sibuti Coral Reefs National Park, Sarawak (Malaysia) to reconst

225 Coral reefs provide essential goods and services but are

226 ration of algae might be expected on Red Sea coral reefs with future ocean warming.

227 Coral reefs worldwide are threatened by thermal stress c

228 rticularly in areas of algal blooms and near coral reefs, as well as in areas affected by oil spills

229 as the cause of devastating disturbances in coral reefs, kelp forests, and rocky shores.

230 Given the catastrophic changes befalling coral reefs, understanding coral gene function is essent

231 y, Southern Taiwan is home to well-developed coral reefs, which frequently experience cold-water intr

232 most prevalent and severe pressures faced by coral reefs.

233 ation in a structurally complex test system: coral reefs.

234 Global change causes widespread decline of coral reefs.

235 in regulating toxic cyanobacteria blooms on coral reefs.

236 on had a high dependence on species that use coral reefs.

237 les in understanding ecological processes on coral reefs.

238 n frameworks aimed at securing the future of coral reefs.

239 blages is greatly reduced on Earth's hottest coral reefs.

240 plore diversity-functioning relationships in coral reefs.

241 itical to corals and other species living in coral reefs.

242 s those caused by the 1997-1998 El Nino, ETP corals reefs have demonstrated regional persistence and

243 sed on live coral, and to identify potential coral refugia in the face of human-driven stressors, inc

244 e-expression changes during heat stress in a coral relative, the sea anemone Aiptasia.

245 lations, and therefore predation pressure on corals, remains limited.

246 T processing technique, previously tested in coral research, is applied to facilitate the characteris

247 he RAS-B system, while flow affected certain coral response variables in the FTS tanks; there were fe

248 To investigate corals' responses to stress and other aspects of their b

249 ift so that seaweeds now dominate previously coral-rich reefs.(6-8) Discovery of the powerful grazing

250 nutrients, they may also help contribute to coral rubble production through physical erosion.

251 However, coral's diel oxygen dynamics and fermentative pathways r

252 pectrometry analyses identified strombine as coral's main fermentative end product.

253 ns of morphological evolution in anthozoans (corals, sea anemones) by examining skeletal traits in th

254 adly, we conclude that CRISPR mutagenesis in corals should allow wide-ranging and rigorous tests of g

255 Historical coral skeleton (CS) delta(18) O and delta(15) N records

256 Fossil coral skeletons also present a rich record that enables

257 While some researchers consider coral skeletons as mainly passive recorders of ocean con

258 ly observed in speleothems and scleractinian coral skeletons is inherited from the dissolved inorgani

259 iomineral growth, isotope incorporation, and coral skeletons' resilience to ocean warming and acidifi

260 Predation by corallivores, such as the short coral snail Coralliophila abbreviata, are one such threa

261 he newly assembled transcriptome of the Cape coral snake reveals that organoids express high levels o

262 on and sample processing during time-limited coral spawning events, facilitating larger-scale and hig

263 a) had higher lethal thermal limits than two coral species (Pocillopora verrucosa and Stylophora pist

264 Second, the coral species had generally greater deactivation energie

265 Because many coral species spawn only once per year during a narrow t

266 wth anomalies and tissue loss-affecting five coral species.

267 cell death is an important component in the coral stress response.

268 igher catches of species that depend on live coral, suggesting that coral area could be used to predi

269 waves by surpassing the thermal threshold of coral survival.

270 All cultured corals survived the 140-day treatment, and the physiolog

271 Unexpectedly, some corals survived the event by recovering from bleaching w

272 ortant to understand the forces that inhibit coral survivorship and recovery.

273 nutrient regimes in ways that could increase corals' susceptibility to further stressors.

274 Loci that mapped to coral, symbiont, and microbial references revealed genet

275 ropogenic nutrients reduced the diversity of coral-symbiotic algal interactions and caused nutrient a

276 reveal common principles by which different corals take up or lose their endosymbionts.

277 Analysis of the abundances of coral taxa in fossil bulk samples define the Historical

278 Across all coral taxa, projected stochastic growth rates (lambda(s)

279 Although live coral tends not to face directly into the prevailing cur

280 ia pertusa is a framework-forming cold-water coral that supports numerous ecosystem services in the d

281 ng, leading to widespread mortality of stony corals that can fundamentally alter reef structure and f

282 ild a "Noah's Ark" biological repository for corals that taps into the network of the world's public

283 ss the ability of both approaches to resolve coral thermotolerance differences reflective of in situ

284 hich mimics morphological features of living coral tissue and the underlying skeleton with micron res

285 olecules, nutrients or nanoparticles through coral tissues are poorly documented.

286 icrobiomes in accentuating phase shifts from coral to algae on tropical reefs.

287 e find that ETP reef recovery patterns allow coral to persist under these El Nino-stressed conditions

288 ariation and therefore the capacity of these corals to adapt may be underappreciated.

289 The potential of reef-building corals to adapt to increasing sea-surface temperatures i

290 al ocean change can affect the resilience of corals to environmental stressors and that exposure to c

291 fs that have moderating turbidity are in the Coral Triangle.

292 ere was a microbial assemblage unique to the coral-turf algae interface displaying higher microbial a

293 there are specific biogeochemical changes at coral-turf algal interfaces that predict the competitive

294 ding ecological and evolutionary dynamics of corals under regimes of increasing environmental disturb

295 on is critical to informing future models of coral vulnerability to inevitable global change, particu

296 This coral was measured in November 2019 as part of an effort

297 Half of the corals were fed Artemia sp. brine shrimp in a separate f

298 ferences across functional groups (algae vs. corals) were apparent for two key thermal performance me

299 biochemical analyses suggest a mechanism in coral which differs from that of humans, where the CARD-

300 The framework consists of mostly live corals with a total area of about 10 m(2) and the length

301 has become a major problem for reef-building corals worldwide.