Results 211 to 220 of about 103,225 (263)
Mutualism on the deep-sea floor: a novel shell-forming sea anemone in symbiosis with a hermit crab. [PDF]
R Soc Open SciYoshikawa A +13 more
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Diverse quorum sensing systems regulate microbial communication and biogeochemical processes in deep-sea cold seeps. [PDF]
MicrobiomePeng J +11 more
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Seamount larval dispersal networks: A potential strategy for conserving ecological connectivity from deep-sea mining. [PDF]
Ecol ApplSaito N +6 more
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Peripheral tissues of deep-sea mussels exhibit autonomous circadian timing via an atypical mechanism
Mat AM +4 more
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2020
Extreme morphologies are often found in extreme conditions. Many commonalities exist in the morphology of deep and shallow-water sea urchins, but different evolutionary histories and adaptations to living at great depths have created peculiar and divergent morphologies within deep-sea sea urchins.
Stevenson, Angela, Kroh, Andreas
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Extreme morphologies are often found in extreme conditions. Many commonalities exist in the morphology of deep and shallow-water sea urchins, but different evolutionary histories and adaptations to living at great depths have created peculiar and divergent morphologies within deep-sea sea urchins.
Stevenson, Angela, Kroh, Andreas
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Deep-sea organisms research oriented by deep-sea technologies development
Science Bulletin, 2022Deep-sea environment, characterized by high pressures, extremely high/low temperatures, limited photosynthesis-generated organic matter, darkness, and high levels of corrosion, is home to flourishing special ecosystems in the world. Here, we illustrate how the deep-sea equipment offers insights into the study of life in the deep sea based on the work ...
Jing-Chun, Feng +5 more
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2014
Deep-sea sediments typically have sedimentation rates less than 30 m/10 years, and rates as low 0.1 m/10 years have been reported. The slow sedimentation rates and unusual sediment compositions reflect the low fluxes of aluminosilicates eroded from continents. The terrigenous material that does deposit is often windblown dust.
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Deep-sea sediments typically have sedimentation rates less than 30 m/10 years, and rates as low 0.1 m/10 years have been reported. The slow sedimentation rates and unusual sediment compositions reflect the low fluxes of aluminosilicates eroded from continents. The terrigenous material that does deposit is often windblown dust.
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Deep-Sea Pleistocene Biostratigraphy
Science, 1966The first detailed paleontological analysis of a deep-sea pistoncore from the Caribbean Sea has been completed. The core, P6304-8, was raised from 3927 meters, east of Beata Ridge at 14°59′N, 69°20′W. Formerly, stratigraphic works in this area were based on studies of paleotemperature, measured by the oxygen isotope mass spectrometry method, or on ...
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Deep sea navigation techniques
Marine Geophysical Researches, 1990Accurate navigation forms an essential part of all research at sea and the deep ocean imposes it’s own unique problems. This chapter discusses several of the techniques in current use on the research vessels of the Natural Environment Research Council (NERC), concentrating on those systems which provide global navigation facilities, as opposed to the ...
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