Composition and biomass of phytoplankton assemblages in coastal Antarctic waters: a comparison of chemotaxonomic and microscopic analyses

By Irene A. Garibotti, M. Vernet, W. Kozlowski, M. Ferrario. 2003

129 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

Dynamics of phytoplankton communities during late summer around the tip of the Antarctic Peninsula (2012, methodology): “Phytoplankton cell abundance and carbon biomass data were calculated for surface samples, as they are representative of the UML (Garibotti et al., 2003).”
Intense stratification leads to phytoplankton nutrient limitation and reduced microzooplankton grazing in the southeastern Bering Sea (2008, unknown): “Occasional values 4200 have been observed in high-latitude ecosystems (Booth and Smith, 1997); in one Antarctic study ( Garibotti et al., 2003 ), the highest C:Chl values were associated with low phytoplankton growth rates and low chlorophyll levels.”
Photoacclimation in phytoplankton: implications for biomass estimates, pigment functionality and chemotaxonomy (2006, result): “Rather, the distribution of Chl a contributed by phytoplankton groups (using HPLC pigment analyses) and C (derived from light microscopy) has been recently compared in several studies (Garibotti et al. 2003; Llewellyn et al. 2005).”
Marine pelagic ecosystems: the West Antarctic Peninsula (2007, background): “The transition from diatoms to flagellates has been attributed to sedimentation (Castro et al. 2002), advection (Moline & Prezelin 1996) and grazing (Garibotti et al. 2003b).”
Phospholipid-derived fatty acids as chemotaxonomic markers for phytoplankton: application for inferring phytoplankton composition (2006, unknown): “In recent years, several studies have compared cell numbers and pigments, and in general a good agreement is found between these 2 methods both in freshwater and marine ecosystems (e.g. Garibotti et al. 2003, Marinho & Rodrigues 2003).”
Seasonal progression of diatom assemblages in surface waters of Ryder Bay, Antarctica (2009, background): “In situ chl a data show high concentrations in the upper water column (above *60 m; Clarke et al. 2008), a pattern typical of Antarctic coastal regions (Garibotti et al. 2003b; Holm-Hansen et al. 1989; Smith et al. 1998).”
Phytoplankton spatial distribution patterns along the western Antarctic Peninsula (Southern Ocean) (2003, methodology): “We also know that in the western Antarctic Peninsula blooms are due to diatoms (Holm-Hansen et al. 1989, Varela et al. 2002, Garibotti et al. 2003).”