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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Relationships between the deep chlorophyll maximum and hydrographic characteristics across the Atlantic, Indian and Pacific oceans</dc:title><dc:creator>Estrada,	Marta	(Avtor)
	</dc:creator><dc:creator>Latasa,	Mikel	(Avtor)
	</dc:creator><dc:creator>Cabello,	Ana Maria	(Avtor)
	</dc:creator><dc:creator>de la Fuente,	Patricia	(Avtor)
	</dc:creator><dc:creator>Guallar,	Carles	(Avtor)
	</dc:creator><dc:creator>Mozetič,	Patricija	(Avtor)
	</dc:creator><dc:subject>Malaspina 2010</dc:subject><dc:subject>chlorophyll a</dc:subject><dc:subject>nitracline</dc:subject><dc:subject>deep chlorophyll maximum</dc:subject><dc:subject>phytoplankton size fractionation</dc:subject><dc:subject>Atlantic Ocean</dc:subject><dc:subject>Pacific Ocean</dc:subject><dc:subject>Indian Ocean</dc:subject><dc:subject>hydrobiology</dc:subject><dc:subject>marine biology</dc:subject><dc:description>The Malaspina-2010 circumnavigation expedition on board R/V Hesperides surveyed tropical and subtropical regions of the Atlantic, Indian and Pacific oceans between December 2010 and July 2011. This article examines the relationships between the distribution of chlorophyll a (Chl a), major inorganic nutrients and other hydrographic variables. A deep chlorophyll maximum (DCM) was found at most stations between 60 and 150 m depth; it occurred close to the level of 1% surface photosynthetically active radiation and was associated with the nitracline. There was a negative relationship between total Chl a at surface and the DCM depth, and between Chl a concentration at the DCM and DCM depth. In terms of Chl a concentration, picophytoplankton was the dominant size class at all sampled light intensities (surface, 20% of surface PAR and PAR at DCM), oceans and geoclimatic zones, except at some stations influenced by upwellings or divergences. Within the Chl a concentration ranges found in this study, the proportion of picophytoplankton increased with total Chl a, in contrast with some previous findings. Vertically integrated Chl a was positively correlated with surface Chl a, with similar slopes for the whole data set and for the different oceans and zones. In turn, surface Chl a and sea surface temperature showed a negative correlation for the Indian Ocean and the subtropical zone, a positive correlation for the Atlantic, and non-significant relationships for the remaining oceans and zones.</dc:description><dc:date>2024</dc:date><dc:date>2025-04-04 10:42:22</dc:date><dc:type>Neznano</dc:type><dc:identifier>21830</dc:identifier><dc:identifier>UDK: 574</dc:identifier><dc:identifier>ISSN pri članku: 1886-8134</dc:identifier><dc:identifier>DOI: 10.3989/scimar.05519.092</dc:identifier><dc:identifier>COBISS_ID: 228680195</dc:identifier><dc:language>sl</dc:language></metadata>
