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Illustration depicting Air-Sea exchanges

Scientists have assumed that under calm conditions, the ocean’s surface layer doesn’t mix with deeper waters. New observations suggest that this may not be true.

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Illustration depicting Air-Sea exchanges

How the Dimethylsulfoniopropionate (DMSP) compound affects the environment

How biomagnification works

Liquid Chromatography – Mass Spectrometry

Sources of dissolved iron in seawater

Illustration depicting the chemical journey of leaf wax

Formation cycle of piteraq winds

Illustration depicting the formation of the Samoan Islands chain

The ocean’s Biological Carbon Pump

Microbial life is discovered in vents

Different stages of photosynthesis

How a biofilm forms in the sea

How a Deep Hypersaline Anoxic Basin (DHAB) forms

The existence of ancient vent microbes

Illustration explaining the life cycle of eels

Galápagos Islands unique ecosystem involving trade winds and EUC

How a DMON buoy operates to detect and transmit right whale location info

How a DMON buoy operates to detect and transmit right whale location info

How a hydrothermal vent system works

How a hydrothermal vent system works

How a Thermal Glider operates autonomously in the ocean

How antibacterial resistant bacteria spreads resistance

How biological compounds from phytoplankton blooms enter the atmosphere

How blue holes are formed

How blue holes are formed

How Cyanobacteria Crocosphaera watsonii recycles iron

How the Fraser River picks up chemical signatures along its journey

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