A dissolved cobalt plume in the oxygen minimum zone of the eastern tropical South Pacific

For the Central Domain, the major sources of moisture for South America are the Atlantic and South Pacific, the North Atlantic and Mediter- ranean for Europe, and the Indian Ocean

central primary plate; RPP- radial primary plate; RS- radial shields; and b) oral view: OS- oral shield; ADS – adoral shield; J- jaw. formed by large and inflated scales with

5a with data collected in the Southern Ocean (Fig. 5b) near the Kerguelen plateau, where natural iron fertilisation of surface waters has clearly been demon- strated (Blain et

The source water masses are Subtropical Water (STW), Subantarctic Water (SAAW), Equatorial Subsurface Water (ESSW), Antarctic Intermediate Water (AAIW) and Pacific Deep Water (PDW).

The winter convection that leads to deep mixed layers in the Subantarctic Zone is the first step in the formation of SAMW, of which southeast Pacific AAIW is the densest

They are understood to mostly originate from sul- fide production in sediments (Fig. To date sulfidic events have been reported from the eastern tropical South Pacific, the Arabian

The two points considered at the alternate sides, of the tangents through the diameter of the circle, and then the line joining these points divides the circle

formation. Based on these data sources we constrain diapycnal mixing in the tropical North Atlantic OMZ, from which we are able to estimate the average diapycnal oxy- gen supply as