Vertical Distribution of Phytoplankton in the Central and Northern Part of the Gulf of California (June 1982)

Abstract

Abstract. Vertical profiles of temperature, nutrients (silicate, phosphate, and nitrate), chlorophyll a and phytoplankton abundance are given for six stations located in the Gulf of California, June 1982, above 1 % of light intensity. The vertical distribution of phytoplankton was related to the water column structure: stratified stations had a defined nutricline and subsurface chlorophyll and phytoplankton abundance maxima were present, which were found to be related to the depth of the principal thermocline; vertical distribution of taxa was not uniform and low affinity values (< 0.5) were calculated among depths at these stations. Despite the irregular vertical distribution of chlorophyll and cell number, there was a great affinity in the species composition throughout the euphotic zone at well‐mixed or weakly stratified stations. Nanoplankton organisms, mainly coc‐colithophorids, were the most important numerical contributors at the chlorophyll maxima, except when this was superficial, in which case diatoms were the most numerous group. Some patterns of the vertical distribution of the main phytoplankton groups (e.g., diatoms, dinoflagellates, and microflagellates) are shown. The spectrum of diversity in the water column was useful only for mixed‐waters. The relationship between stability, nutrients, and phytoplankton ‐ regarding their vertical distribution ‐ and the importance of physical and biological processes on phytoplankton ecology are discussed.