North African dust is an important (but not dominant) source of iron to the Gulf of Mexico
Hayes and colleagues have combined data to estimate how important North African dust could be as a source of iron to the Gulf of Mexico.
Some recent GEOTRACES science findings are reported below.
Hayes and colleagues have combined data to estimate how important North African dust could be as a source of iron to the Gulf of Mexico.
Lemaitre and her colleagues realized the simultaneous analysis of the dissolved nickel isotopes and concentrations in the North Atlantic.
They provide an updated mass balance of the Arctic land and ocean mercury cycle.
They synthesized what controls the barium distribution in the Arctic Ocean.
In this study, radium is used as a tracer for the waters of the Amazon that mix with those of the Atlantic Ocean.
A suite of trace element was measured in aerosols collected in the North and equatorial Pacific.
They have developed optical sensors for particulate inorganic carbon concentration.
They established the distribution of titanium in Amazon and Pará rivers and their related plume during the high discharge period.
Their findings highlight the importance of the Transpolar Drift in delivering dissolved silica and iron to feed low diatom primary production in the central Arctic Ocean.