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1 oretical yield from the sugar composition in macroalgae).
2 esilience of coral reefs suffering blooms of macroalgae.
3 that OA may enhance the allelopathy of some macroalgae.
4 bove that needed to prevent proliferation of macroalgae.
5 ornia, a habitat rich in alginate-containing macroalgae.
6 of a functional xanthophyll cycle in a green macroalgae.
7 nine reefs underwent regime shifts to fleshy macroalgae.
8 icient, sustainable feedstocks such as brown macroalgae.
9 e bacteria, fungi, microalgae, and spores of macroalgae.
10 ble of producing ethanol directly from brown macroalgae.
11 e nutrients may help facilitate increases in macroalgae.
12 re was no evidence for regional increases in macroalgae.
13 evidence that urchins control the biomass of macroalgae.
14 reef health is characterized by increases in macroalgae.
15 rpene-benzoic acids and diterpene-phenols in macroalgae.
16 damage, disease, and increasing abundance of macroalgae.
17 icane damage, and an increasing abundance of macroalgae.
18 were codominant to a community dominated by macroalgae.
19 y for CO2:HCO3(-) use (delta(13)C values) of macroalgae along a gradient of CO2 at a volcanic seep, a
20 heterotrophic microbial overgrowth of coral, macroalgae also directly harm the corals via hydrophobic
21 sity, likely mediated by competition between macroalgae and corals, suggesting that fish excretion ma
22 (Ulva intestinalis), as recruitment of both macroalgae and diatoms were favored in elevated nutrient
24 a major cell wall polysaccharide from marine macroalgae and nutrient source for heterotrophic bacteri
28 anagement action to both forestall shifts to macroalgae and preserve properties essential for resilie
29 a feature shared with the cell walls of all macroalgae and that is important for ion homoeostasis, n
30 requires an understanding of the effects on macroalgae and their grazers, as these underpin the ecol
31 presence of top-down control on urchins and macroalgae, and (2) lobster fishing triggers a trophic c
32 iodine concentrations were detected in green macroalgae ( approximately 0.005% DW), implying that qua
38 In comparison to the seaward algal zone, macroalgae are rare in the urchin zone, where the densit
39 sed platform, which enabled the use of brown macroalgae as a feedstock for the production of biofuels
44 communities have quantified rapid removal of macroalgae by herbivorous fishes, yet how these findings
45 indings indicate that the application of the macroalgae C. linum could represent an effective wastewa
46 results show that all major sugars in brown macroalgae can be used as feedstocks for biofuels and va
47 demonstrates the feasibility of cultivating macroalgae Chaetomorpha linum in different types of muni
49 s, Porphyra sp. and Osmundea pinnatifida are macroalgae consumed as food in some of the Azorean Islan
52 bromoperoxidase protein from the marine red macroalgae Corallina officinalis has been determined by
53 cilaria vermiculophylla and Chondrus crispus macroalgae cultivated in the Portuguese coast was carrie
55 under present-day conditions, (ii) that two macroalgae damage corals via allelopathy, and (iii) that
56 ield experiments demonstrating that numerous macroalgae directly damage corals by transfer of hydroph
57 highest over areas dominated by seagrass and macroalgae (dissolved DMS/P) and phytoplankton (particul
59 d a yield of 0.281 weight ethanol/weight dry macroalgae (equivalent to ~80% of the maximum theoretica
60 e we found a sharp herbivory threshold where macroalgae escape control, ambient levels of herbivory b
62 sing the effect of climate-related stress on macroalgae from being positive to negative had no influe
64 ibution in nature, where they are present in macroalgae, fungi, and bacteria, but have been exclusive
66 In contrast to other studies of calcified macroalgae, however, we observed an increase in the abun
67 d fossil fuel resources are depleted, marine macroalgae (i.e., seaweed) is receiving increasing atten
68 nans, major cell wall polysaccharides of red macroalgae, in the marine heterotrophic bacterium Zobell
70 n and enrichment of phlorotannins from Irish macroalgae is vital to facilitate the use of this valuab
73 ogenic organic iodine compounds emitted from macroalgae may be responsible for coastal particle burst
75 m solid-liquid extracts (SLE) of three brown macroalgae, namely Fucus spiralis Linnaeus, Pelvetia can
76 pounds present in ethanolic extracts from 18 macroalgae of the Portuguese coast were analysed by gas
78 to elevated CO2 is hypothesised to advantage macroalgae over corals, contributing to these shifts, bu
79 ated the spatiotemporal response of tropical macroalgae (Padina sp., Amphiroa sp. and Turbinaria sp.)
80 effects of hydrophobic surface extracts from macroalgae paralleled effects of whole algae; both findi
81 ce of benthic invertebrates suggest that the macroalgae played a key structuring role in these commun
82 he lack of recalcitrant lignin components in macroalgae polysaccharide reserves provides a facile rou
83 obster (predator), sea urchins (grazer), and macroalgae (primary producer) in giant kelp forest commu
84 in coral-algae interactions; turf algae and macroalgae promote heterotrophic microbial overgrowth of
91 t contribution for the valorisation of these macroalgae species as sources of valuable phytochemicals
93 and extensive biomass of alginate-containing macroalgae, the observed bacterial dynamics associated w
94 f ecosystem lies in relation to the coral-to-macroalgae tipping point is fundamental to understanding
95 , potentially due to low grazer affinity for macroalgae (Ulva intestinalis), as recruitment of both m
97 enables bioethanol production directly from macroalgae via a consolidated process, achieving a titer
98 rove the herbivore richness effects, because macroalgae were unable to effectively deter fishes with
99 o particle formation from Laminaria digitata macroalgae were undertaken to elucidate aerosol formatio
100 caused a fourfold reduction in the cover of macroalgae, which, because they are the principal compet
101 igate calcifying species, and non-calcareous macroalgae whose CO2 use did not increase consistently w
102 lnerable to OA, and it is likely that fleshy macroalgae will dominate in a higher CO2 ocean; therefor
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