Deep Ocean
The Deep Ocean Density Structure at the Last Glacial Maximum: What Was It and Why?
257
Glacial-interglacial atmospheric CO 2change: a possible “standing volume” effect on deep-ocean carbon sequestration
14
The evolution of deep ocean chemistry and respired carbon in the Eastern Equatorial Pacific over the last deglaciation
15
Overturning circulation driven by breaking internal waves in the deep ocean
5
Deep ocean ventilation, carbon isotopes, marine sedimentation and the deglacial CO 2rise
30
A review of the role of submarine canyons in deep-ocean exchange with the shelf
14
The role of the North Atlantic overturning and deep ocean for multi-decadal global-mean-temperature variability
13
Effect of the salts of deep ocean water on the production of cordycepin and adenosine of Cordyceps militaris-fermented product
9
Seawater capacitance – a promising proxy for mapping and characterizing drifting hydrocarbon plumes in the deep ocean
6
Deep ocean mineral water accelerates recovery from physical fatigue
7
Sensitivity of deep ocean biases to horizontal resolution in prototype CMIP6 simulations with AWI-CM1.0
22
Picocyanobacteria and deep-ocean fluorescent dissolved organic matter share similar optical properties
12
Genomes of Abundant and Widespread Viruses from the Deep Ocean
9
Deep-float salinity data synthesis for deep ocean state estimation: method and impact
8
A Comparison of the Growth Characteristics of Arthrospira platensis in Deep Ocean Water, Surface Ocean Water, and Artificial Ocean Water
8
Different Approaches to International Regulation of Exploitation of Deep-Ocean Ferromanganese Nodules
17
The eruption of submarine rhyolite lavas and domes in the deep ocean Havre 2012, Kermadec Arc
20
Massive upward displacement in the deep ocean
7
Deep ocean exchange with west-European shelf seas
14
Review study of the requirements for deep ocean remote handling equipment
154