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Storm waves are broken by the reef, and the extreme level of wave energy capable of moving boulders is limited to within 200 m of the reef crest because of the short wavelength of storm waves (Goto et al. 2009).
Indeed, increasing doses of exogenous Brk1 restored gradually the normal level of Wave complexes (Fig. 6A).
A more likely explanation is that beach type correlates with some other aspect of the physical environment that A. gazella and A. tropicalis prefer, such as access to water, slope, level of wave action, shade or exposure.
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The study shows that eutrophication-related community shifts on rocky shores may occur very rapidly, regardless of the level of wave-energetic stress and the abundance of grazers, if the nutrient concentrations are high and the colonisation and growth of opportunistic algae are facilitated by disturbance such as (naturally or anthropogenically driven) canopy gap forming processes.
These responses depend on the inhomogeneity level of waves considered.
With the set levels of wave power, nearly all energy is deposited into the ions.
The restoration of normal levels of Wave complexes when Brk1 trimers are supplied indicates that this form comes before the assembled complex.
Moreover, levels of Wave 2 complex components other than Abi1 were unchanged in cells expressing active vs. inactive Rac1 regardless of which Abi1 isoform was expressed (Fig. 4A).
This depended on whether there was also a correlation between ABP and ICP wave amplitudes and on the average level of ICP wave amplitude.
However, the researchers are fairly confident that this is not the case because the monks who had spent the most years meditating had the highest level of gamma wave activity.
Nevertheless, the increase in particle fluxes was not observed till early morning of 9 October in spite of high level of chorus wave activity observed before.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com