ライフサイエンスコーパス: macroalgae

1 oretical yield from the sugar composition in macroalgae).

2 the main monosaccharide constituents of red macroalgae.

3 reef health is characterized by increases in macroalgae.

4 rpene-benzoic acids and diterpene-phenols in macroalgae.

5 damage, disease, and increasing abundance of macroalgae.

6 icane damage, and an increasing abundance of macroalgae.

7 were codominant to a community dominated by macroalgae.

8 ccharides derived from the cell walls of red macroalgae.

9 and increased cyanobacteria, fire coral, and macroalgae.

10 an contribute fixed nitrogen (N) to the host macroalgae.

11 -1) (dw) x h(-1) ) than observed with living macroalgae.

12 da (Yukon Territory) that preserves cm-scale macroalgae.

13 sed on the role of 'browsers' in extirpating macroalgae.

14 and sphingolipids with varied content among macroalgae.

15 d iota composition in different forms of raw macroalgae.

16 ng recruitment or transitions to longer turf/macroalgae.

17 algal communities begin with more turf than macroalgae.

18 ecapod crustaceans, polychaete annelids, and macroalgae.

19 esilience of coral reefs suffering blooms of macroalgae.

20 that OA may enhance the allelopathy of some macroalgae.

21 bove that needed to prevent proliferation of macroalgae.

22 ornia, a habitat rich in alginate-containing macroalgae.

23 of a functional xanthophyll cycle in a green macroalgae.

24 nine reefs underwent regime shifts to fleshy macroalgae.

25 icient, sustainable feedstocks such as brown macroalgae.

26 e bacteria, fungi, microalgae, and spores of macroalgae.

27 ble of producing ethanol directly from brown macroalgae.

28 (Ulva linza) and red (Porphyra umbilicalis) macroalgae.

29 e nutrients may help facilitate increases in macroalgae.

30 re was no evidence for regional increases in macroalgae.

31 evidence that urchins control the biomass of macroalgae.

32 In addition, labelled macroalgae ((13) C), previously exposed to elevated CO(2

33 Fleshy macroalgae (2-66% of cover), algal turfs (0-47%), and sp

34 ard chemical cues produced by Laurencia spp. macroalgae, a known settlement cue for the species.

35 photosynthetic production and growth for two macroalgae; a culturally valued native (Ulva lactuca) an

36 The macroalgae addition resulted in an orange, darker and le

37 (ALs) catalyze the depolymerization of brown macroalgae alginates, widely used naturally occurring po

38 ave exposure gradients suggested that canopy macroalgae allow species with ranges centred in cooler t

39 y for CO2:HCO3(-) use (delta(13)C values) of macroalgae along a gradient of CO2 at a volcanic seep, a

40 heterotrophic microbial overgrowth of coral, macroalgae also directly harm the corals via hydrophobic

41 d in alkali and hydrothermal pretreatment of macroalgae, although seawater led to relatively higher y

42 Ulva zoospores are widespread marine macroalgae and a common organism found in biofouling com

43 Agars are sulfated galactans from red macroalgae and are composed of a d-galactose (G unit) an

44 cture this recruitment by directly consuming macroalgae and coral recruits or by indirectly altering

45 sity, likely mediated by competition between macroalgae and corals, suggesting that fish excretion ma

46 (Ulva intestinalis), as recruitment of both macroalgae and diatoms were favored in elevated nutrient

47 despread life history among animals, plants, macroalgae and fungi, the sexually produced offspring (g

48 and Papua New Guinea, focussing on abundant macroalgae and grazing sea urchins.

49 n the biofilm among sand grains, but also on macroalgae and ice within which it can likely survive lo

50 sociated with multicellular organisms except macroalgae and is abundant in marine waters and surface/

51 a major cell wall polysaccharide from marine macroalgae and nutrient source for heterotrophic bacteri

52 bers of time series of cover of hard corals, macroalgae and other components.

53 Macroalgae and phytoplankton were the two major food sou

54 e methionine (Met) transamination pathway as macroalgae and phytoplankton(10).

55 ion of CHBr(3) from marine organisms such as macroalgae and phytoplankton.

56 tic lineage that includes unicellular algae, macroalgae and plant parasites.

57 rtugal to Norway, but CTI for communities of macroalgae and plant species changed less than those com

58 anagement action to both forestall shifts to macroalgae and preserve properties essential for resilie

59 on with natural ingredients like iodine-rich macroalgae and selenized-yeast is an excellent strategy

60 acid and dimethylallyl pyrophosphate in red macroalgae and show that the biosynthetic genes are co-c

61 ation, with a possible regime shift favoring macroalgae and specialized species of microalgae.

62 a feature shared with the cell walls of all macroalgae and that is important for ion homoeostasis, n

63 requires an understanding of the effects on macroalgae and their grazers, as these underpin the ecol

64 at affect the health and abundance of marine macroalgae and their microbiomes.

65 presence of top-down control on urchins and macroalgae, and (2) lobster fishing triggers a trophic c

66 The archived samples-tree leaves, marine macroalgae, and marine and limnic mussels-represent natu

67 synthesis by marine bacteria, phytoplankton, macroalgae, and some invertebrate animals, and both may

68 iodine concentrations were detected in green macroalgae ( approximately 0.005% DW), implying that qua

69 shallowest reefs (~ 17 m deep) where fleshy macroalgae are abundant together with higher siltation o

70 The most abundant sugars in macroalgae are alginate, mannitol, and glucan, and altho

71 Calcareous macroalgae are highly vulnerable to OA, and it is likely

72 Marine macroalgae are important indicators of healthy nearshore

73 Compared to microalgae, macroalgae are larger in size, thereby imposing lower se

74 The lipophilic fraction of the studied macroalgae are mainly constituted by fatty acids (110.1-

75 Here, we show that (i) three common macroalgae are more damaging to a common coral when they

76 In this regard, multicellular macroalgae are more suitable for harvesting.

77 In comparison to the seaward algal zone, macroalgae are rare in the urchin zone, where the densit

78 Multicellular red algae (or macroalgae) are one of the earliest diverging eukaryotic

79 logical states, such as shifts from coral to macroalgae, are becoming more common.

80 Seaweeds, or marine macroalgae, are valuable renewable resources widely used

81 This study advocates the use of macroalgae as a bioindicator of nitrogen effluent in the

82 sed platform, which enabled the use of brown macroalgae as a feedstock for the production of biofuels

83 This study elevated the potential of brown macroalgae as an emerging reservoir of bioactive lipids

84 The full potential of brown macroalgae as feedstocks for commercial-scale fuel ethan

85 nd polyphenols) valorization of the invasive macroalgae Ascophyllum nodosum within a green biorefiner

86 to compare fucoxanthin content in four brown macroalgae, Ascophyllum nodosum, Fucus serratus, Fucus v

87 Species of temperate macroalgae at their southern limits in the Iberian Penin

88 cooled, fish moved into shallow seagrass and macroalgae beds that were previously out-of-bounds.

89 scading effects of propagule supply on prey (macroalgae) biomass.

90 literature data suggesting that heavy metal macroalgae biomonitoring may be species-specific.

91 his study represents the first comprehensive macroalgae biomonitoring study of metal contamination fr

92 e realized niche area of 43.8 million km(2), macroalgae blooms in the tropical Atlantic and western P

93 Like other marine macroalgae, brown seaweeds are known to accumulate the h

94 Many are functionally dominated by macroalgae, but this community state represents only one

95 communities have quantified rapid removal of macroalgae by herbivorous fishes, yet how these findings

96 indings indicate that the application of the macroalgae C. linum could represent an effective wastewa

97 results show that all major sugars in brown macroalgae can be used as feedstocks for biofuels and va

98 demonstrates the feasibility of cultivating macroalgae Chaetomorpha linum in different types of muni

99 Extracts from the macroalgae Chlorodesmis fastigiata and Amansia glomerata

100 yomes of diverse brown, red and green marine macroalgae collected from polar (Baffin Island), cold-te

101 s, Porphyra sp. and Osmundea pinnatifida are macroalgae consumed as food in some of the Azorean Islan

102 Macroalgae contribute approximately 15% of the primary p

103 Macroalgae contribute substantially to primary productio

104 bromoperoxidase protein from the marine red macroalgae Corallina officinalis has been determined by

105 cilaria vermiculophylla and Chondrus crispus macroalgae cultivated in the Portuguese coast was carrie

106 Extraction of protein from macroalgae, currently defined as "novel food", is challe

107 However, the extent to which macroalgae damage corals directly, the mechanisms involv

108 under present-day conditions, (ii) that two macroalgae damage corals via allelopathy, and (iii) that

109 ved organic matter and herbivorous fishes on macroalgae-derived organic matter to a much higher exten

110 ield experiments demonstrating that numerous macroalgae directly damage corals by transfer of hydroph

111 highest over areas dominated by seagrass and macroalgae (dissolved DMS/P) and phytoplankton (particul

112 ng ecological shifts from hard coral towards macroalgae dominated reefs.

113 epora) under field conditions on a degraded, macroalgae-dominated reef.

114 Tidally exposed macroalgae emit large amounts of I(2) and iodocarbons th

115 d a yield of 0.281 weight ethanol/weight dry macroalgae (equivalent to ~80% of the maximum theoretica

116 e we found a sharp herbivory threshold where macroalgae escape control, ambient levels of herbivory b

117 r bag decomposition experiments with various macroalgae, especially those with high (> 10) C:N ratios

118 va spp is becoming an increasingly important macroalgae for aquaculture.

119 in turn affect other species that depend on macroalgae for resources or habitat structure.

120 sing the effect of climate-related stress on macroalgae from being positive to negative had no influe

121 Rankings of macroalgae from most to least allelopathic were similar

122 ecognized as a key interaction that can keep macroalgae from outcompeting coral.

123 ibution in nature, where they are present in macroalgae, fungi, and bacteria, but have been exclusive

124 Coral cover has declined on many reefs, and macroalgae have increased on some.

125 i.e., phytoplankton) and larger algae (i.e., macroalgae) have increased in certain coastal and open o

126 In contrast to other studies of calcified macroalgae, however, we observed an increase in the abun

127 d fossil fuel resources are depleted, marine macroalgae (i.e., seaweed) is receiving increasing atten

128 Although some collections include macroalgae (i.e., seaweeds), they are relatively few and

129 questions included the role of carbonate and macroalgae in BC cycling, and the degree to which greenh

130 marine food webs, generally spawn on marine macroalgae in shallow nearshore areas that are dispropor

131 The rise of eukaryotic macroalgae in the late Mesoproterozoic to early Neoprote

132 nans, major cell wall polysaccharides of red macroalgae, in the marine heterotrophic bacterium Zobell

133 Algae, especially macroalgae, increased in abundance until they effectivel

134 palatability compared to naturally-occurring macroalgae, influencing herbivory.

135 mbined effects of increasing heat stress and macroalgae intensified coral loss.

136 Farming of macroalgae is a common practice in tropical settings and

137 Macroalgae is an under-utilised tool as a bioindicator o

138 ence of the diversification and expansion of macroalgae is limited by a biased fossil record.

139 n and enrichment of phlorotannins from Irish macroalgae is vital to facilitate the use of this valuab

140 Nonetheless, macroalgae lipidome has been poorly unraveled due to lip

141 Although seagrasses and marine macroalgae (macro-autotrophs) play critical ecological r

142 nd in alginate, a major constituent of brown macroalgae, making it a valuable tool for the selective

143 The farmed macroalgae may also differ in palatability compared to n

144 In the reef system, seagrass and macroalgae may be more important benthic producers of di

145 ogenic organic iodine compounds emitted from macroalgae may be responsible for coastal particle burst

146 This research suggests that macroalgae may use DMSP to maintain metabolic function d

147 -HTau) of 26 different species of commercial macroalgae, microalgae and 10 algae-enriched food produc

148 , hard coral and, to a lesser extent, fleshy macroalgae microhabitats.

149 m solid-liquid extracts (SLE) of three brown macroalgae, namely Fucus spiralis Linnaeus, Pelvetia can

150 Green macroalgae of the genus Ulva play a key role in coastal

151 pounds present in ethanolic extracts from 18 macroalgae of the Portuguese coast were analysed by gas

152 event, as evidenced by benthic phototrophic macroalgae of the Songluo Biota preserved in black shale

153 of grazing fishes and reduce the coverage of macroalgae on coral reefs.

154 nerability to and reversibility of shifts to macroalgae on coral reefs.

155 dy investigated the effects of 67 species of macroalgae on methanogenesis and rumen fermentation in v

156 Local factors such as high abundance of macroalgae or urchins magnified coral loss in the year a

157 ted into the benthic community, we collected macroalgae over 10 days following the storm and measured

158 to elevated CO2 is hypothesised to advantage macroalgae over corals, contributing to these shifts, bu

159 ated the spatiotemporal response of tropical macroalgae (Padina sp., Amphiroa sp. and Turbinaria sp.)

160 effects of hydrophobic surface extracts from macroalgae paralleled effects of whole algae; both findi

161 Understory macroalgae partly compensated for canopy NPP losses and

162 on fish community composition and coral and macroalgae percentage cover between 2006 and 2017 from 5

163 ce of benthic invertebrates suggest that the macroalgae played a key structuring role in these commun

164 he lack of recalcitrant lignin components in macroalgae polysaccharide reserves provides a facile rou

165 obster (predator), sea urchins (grazer), and macroalgae (primary producer) in giant kelp forest commu

166 in coral-algae interactions; turf algae and macroalgae promote heterotrophic microbial overgrowth of

167 ds protection, coastal wetlands restoration, macroalgae protection, macroalgae restoration, seafloor

168 Calcifying coralline macroalgae provide biogenic habitats colonised by epiphy

169 he marine environment, seaweeds (i.e. marine macroalgae) provide a wide range of ecological services

170 e composition and properties of the invasive macroalgae R. okamurae and explore potential application

171 ing possible tipping points in the herbivory-macroalgae relationships has remained a challenge.

172 Brown macroalgae represent a sustainable and abundant source o

173 Brown macroalgae represent an ideal source for complex polysac

174 These macroalgae represent promising natural bioactive sources

175 wetlands restoration, macroalgae protection, macroalgae restoration, seafloor protection, and seaweed

176 omote the understanding of carbon cycling in macroalgae-rich waters worldwide.

177 ive lipidomic analysis was performed in four macroalgae: Saccharina latissima, Fucus vesiculosus, Fuc

178 A total of 831 macroalgae samples of Fucus vesiculosus and Ulva sp. wer

179 The pelagic brown macroalgae Sargassum spp. have grown for centuries in ol

180 ritical, habitat-forming foundation species (macroalgae, seagrass, corals) to marine heatwaves in 132

181 hemical composition and bioactivity of three macroalgae (seaweed) species: Palmaria palmata, Ascophyl

182 transport and concurrent growth of nearshore macroalgae (seaweed), followed by their export into the

183 y, regional populations have consumed edible macroalgae seaweeds containing unique polysaccharides.

184 Macroalgae (seaweeds) are the subject of increasing inte

185 Prospecting macroalgae (seaweeds) as feedstocks for bioconversion in

186 SEM images of hydrolyzed macroalgae showed that reverse-osmosis water caused cont

187 t contribution for the valorisation of these macroalgae species as sources of valuable phytochemicals

188 rtions by 7 and 24%, respectively, whereas 3 macroalgae species decreased molar proportion of butyrat

189 Thirty one samples from different macroalgae species have been studied to determine the in

190 Elevated carbon-to-nitrogen ratios among macroalgae suggested that competition for nitrogen also

191 using acetylene reduction assays with living macroalgae surrounding Santa Catalina Island were low (m

192 omparable dark and light BNF rates with most macroalgae surveyed suggest macroalgal detrital systems

193 rameworks, deriving rare earth elements from macroalgae, synthetic gene drives in plants, and low-emi

194 icrobes in coastal environments benefit from macroalgae that annually release ~10(14) g of carbon,(15

195 ding algal flavonoids, which are produced by macroalgae that Roseovarius species associate with.

196 and extensive biomass of alginate-containing macroalgae, the observed bacterial dynamics associated w

197 assum, and the means by which these floating macroalgae thrive in the nutrient-poor waters of the ope

198 f ecosystem lies in relation to the coral-to-macroalgae tipping point is fundamental to understanding

199 More modest changes in macroalgae, turf algae, and sponge cover were also obser

200 two coral species and three types of algae (macroalgae, turfing microalgae, and crustose coralline a

201 report on a non-thermal, chemical-free green macroalgae Ulva sp. protein extraction by osmotic shock

202 , potentially due to low grazer affinity for macroalgae (Ulva intestinalis), as recruitment of both m

203 ol and alpha-tocopherol in New Zealand brown macroalgae, Undaria pinnatifida, were investigated.

204 enables bioethanol production directly from macroalgae via a consolidated process, achieving a titer

205 or and microstructural features of the dried macroalgae were also evaluated, as well as their nutriti

206 No other macroalgae were identified as potential mitigants of ent

207 automated gas production system for 24-h and macroalgae were tested at 2% (feed dry matter basis) inc

208 rove the herbivore richness effects, because macroalgae were unable to effectively deter fishes with

209 o particle formation from Laminaria digitata macroalgae were undertaken to elucidate aerosol formatio

210 ntration was decreased between 5 and 8% by 3 macroalgae, whereas AT reduced it by 10%.

211 ccupation for months of open ocean waters by macroalgae, which do not naturally occur there, will pro

212 caused a fourfold reduction in the cover of macroalgae, which, because they are the principal compet

213 ores play in preventing the establishment of macroalgae, while less research has focused on the role

214 igate calcifying species, and non-calcareous macroalgae whose CO2 use did not increase consistently w

215 nvestigating the taphonomy of well-preserved macroalgae will aid in identifying these target environm

216 lnerable to OA, and it is likely that fleshy macroalgae will dominate in a higher CO2 ocean; therefor

217 sulfated polysaccharide isolated from brown macroalgae with a broad range of biological properties;

218 what is typically reported for other marine macroalgae, with a bimodal distribution.