Primary productivity estimation in two seamounts in the southern Gulf of California, México.

Authors

  • G. Verdugo-Dí­az
  • R. Cervantes Duarte
  • M. O. Albáñez-Lucero

DOI:

https://doi.org/10.37543/oceanides.v23i1-2.43

Keywords:

Primary Productivity, Gulf of California, El Bajo Gorda

Abstract

Vertical profiles of temperature and natural fluorescence from 100 m deep were made during February 2005. Water transparency was measured using Secchi’s disc, as well samples of superficial water and at maximum of fluorescence deep were collected to analyze inorganic nutrients. In “El Bajo
Espiritu Santo” temperature (20 °C at surface)
diminished gradually with depth, without significant stratification.Primary productivity shows superficial values close to 6 mg C m-3 h-1, reaching  undetectable values at 20 m of depth. In “El Bajo Gorda” surface temperature reached 22 °C and the water column shows a thermocline between 35 m and 45 m of depth. The profiles of primary productivity presented a subsurface maximum (approximately 2 mg C m -3 h-1) associated with the thermocline.

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Published

2008-12-31

How to Cite

Verdugo-Dí­az, G., Cervantes Duarte, R., & Albáñez-Lucero, M. O. (2008). Primary productivity estimation in two seamounts in the southern Gulf of California, México. CICIMAR Oceánides, 23(1-2), 39–43. https://doi.org/10.37543/oceanides.v23i1-2.43

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