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Titlebook: Ecological Impacts of Tsunamis on Coastal Ecosystems; Lessons from the Gre Jotaro Urabe,Tohru Nakashizuka Book 2016 Springer Japan 2016 Tsu

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楼主: Gratification
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Official Corruption in the Reform Era, The tsunami had an overall significant negative impact on the rocky intertidal community at the regional scale, although the negative impact seemed smaller than those of similar large-scale disturbances on rocky intertidal communities. There was a significant negative impact of the tsunami on mobil
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3D-CFD-Modeling of the Wall Heat-Transfer,nd around the lower limit of the species’ normal vertical range decreased, and consequently, the zonation returned almost to the state before the earthquake by July 2013. During the study period, the population dynamics of this barnacle were driven in complex ways by interactions among larval supply
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https://doi.org/10.1007/978-3-030-91471-4 event (i.e., the tsunami, estuary closing, and typhoon). Macrozoobenthic density recovered within 6 months after the tsunami and typhoon, chiefly due to the density overshoots of several opportunistic taxa. Though tsunami- and typhoon-induced changes in macrozoobenthic community structure were sign
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An Insight into Mergers and Acquisitionscobbles) and secondary substrates (e.g., oyster’s and algal bodies) both contributed to increased species richness and population density. Although direct-developing species, which lack planktonic larval stages, had hardly been expected to colonize the restored and newly created vacant tidal flats,
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https://doi.org/10.1007/978-3-031-44416-6idered threatened (according to the Japanese Association of Benthology) appeared in these and newly created tsunami-flooded habitats after 2011. Our data suggest that the marine macrobenthos in this region, including these threatened taxa, were tolerant of the tsunami disturbance or comprised opport
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Maria Speranza,Halil Çakan,Lucia Ferronirvival of clams. The tsunamis have also contributed to dispersion of benthic organisms. For example, the redistribution of oysters across the mud bottom increased their range. In addition to these events, land subsidence resulted in marked changes to the vertical position of the intertidal zone. The
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https://doi.org/10.1007/978-90-481-2655-2instead of them, but they quickly recovered for 2 or 3 years. By contrast, in the shallow sea of Sendai Bay, only . increased at 1 year after the tsunami (July to November 2012), but mean individual density of bivalves decreased 2 years after the tsunami (March 2013). In the shallow sea, the recover
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