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Determining the basic processes governing the biogeochemical structure of the water column is a key challenge for today's oceanographers. Knowledge of these basic processes for an aquatic system makes...
Uppermost Holocene (Unit 1) microlaminated sediments of the deep central Black Sea, which accumulate at ca. 0.02 cm/y, are a classic natural laboratory for exploring geochemical proxies used to identi...
Strength in Diversity     Diversity  Oceanography Society       2015/7/27
On Inauguration Day 2005, the TOS Council, the governing board of The Oceanography Society, held its Annual Meeting by teleconference. Council members dialed in from five different time zones. This wa...
I love teaching the first course in oceanography for non-majors—indeed, that is my professional specialty. Some readers of this column may look upon an assignment to teach a freshman general oceanogra...
he recent monograph edited by Jonathan Bamber and Tony Payne is an excellent resource for those researchers wishing to learn about the status of the modern cryosphere and its influence on global clima...
The hydrogeology of the oceanic crust influences numerous global processes and properties, including the thermal evolution of oceanic lithosphere, crustal alteration and the chemistry of crustal fluid...
Time is of the Essence     Time  the Essence       2015/7/24
From the age of the Earth itself, to the rates at which mountains erode and species evolve, time and rates of change have been the "holy grail" of geologic knowledge. In the study of sedimentary layer...
The Deep Sea Drilling Project (DSDP; 1966–1983) and the Ocean Drilling Program (ODP; 1983–2003) have supplied an amazing amount of information used in reconstruction of past climates, and the present ...
Subduction zones have been consuming oceanic lithosphere since the dawn of plate tectonics on this planet (Figure 1). Raw materials such as pelagic and terrigenous sediments, altered and fresh basalti...
Short-lived El Niño events are temporary changes in tropical Pacific conditions that are responsible for dramatic perturbations to "normal" tropical climate, such as drought in Indonesia and floo...
Certain low-molecular-weight gases, such as methane, ethane, and carbon dioxide, can combine with water to form ice-like substances at high pressure or low temperature. These compounds, commonly calle...
The Arctic Ocean is a small, nearly landlocked ocean basin that is the shallowest in the world (Figure 1). It has maintained a polar location since forming in Early Cretaceous times (Grantz et al., 19...
A rich mosaic of disparate crustal types characterizes the Earth beneath the sea. Although "normal" oceanic crust approximately 7-km thick is by far the most prevalent, abnormally thick oceanic-type c...
Since the inception of the Deep Sea Drilling Project (DSDP) and during the Ocean Drilling Program (ODP), scien-tific ocean drilling has been almost wholly confined to outer-shelf water depths or great...
Knowledge of the composition of oceanic crust is critical for calculating the fluxes of mass, heat, and volatiles from Earth's interior to its crust, oceans, and atmosphere. In the great debate over c...

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