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1 sites expelling methane-rich fluids from the seabed.
2 ens of millions of years after burial in the seabed.
3 igh activity under extreme conditions in the seabed.
4 ng indirect evidence that they swam near the seabed.
5 ail to sample this critical component of the seabed.
6 f the upper ocean's productivity to the deep seabed.
7 tion, potential pore water saturation in the seabed, and the potential occurrence of secondary reacti
17 living fish and a profound reorganization of seabed ecosystems since the nineteenth century industria
18 sediments from a range of continental shelf seabed environments and their current and predicted stab
21 ospheric variability and local ice shelf and seabed geometry play fundamental roles in determining th
22 that the observed impacts resulted from high seabed ground accelerations driven by the air gun signal
24 ng benthic prey composition through physical seabed impacts and (ii) by removing overall benthic cons
27 chaeal communities inhabiting the subsurface seabed live under strong energy limitation and have grow
28 of trawling impacts on whole communities of seabed macroinvertebrates on sedimentary habitats and de
36 ing 6% of biota per pass and penetrating the seabed on average down to 2.4 cm, whereas hydraulic dred
38 degradation of organic matter in the anoxic seabed proceeds through a complex microbial network in w
39 ely accumulating on modern land surfaces and seabeds, provide unique information on the status of pre
42 ing importance as humankind moves to exploit seabed resources in ever-deepening waters of coastal oce
43 nthic biological baseline surveys for the UK Seabed Resources Ltd. exploration contract area (UK-1)
44 ter temperatures at intermediate depth, as a seabed ridge blocks the deepest and warmest waters from
46 In this study we use a slo-corer to collect seabed samples with an undisturbed surface layer and a G
47 istance from haul out, proportion of sand in seabed sediment, and annual mean power were important pr
48 to hydrodynamic measurements and analyses of seabed sediments, the period when bed shear stress due t
50 the bryozoan Fenestrulina rugula) dominating seabed spatial cover and drove a reduction in overall di
53 transects perpendicular to the bank margin, seabed temperature change at individual sites ranged fro
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