Video plankton recorder reveals high abundances of colonial Radiolaria in surface waters of the central North Pacific

By M. Dennett, David A. Caron, Anthony F. Michaels, Scott Gallager, C. Davis. 2002

90 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/cee7e91c0206290f8fb0c5b9c4ad8b8376f1fbd9

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Citations in the corpus

A three‐axis fast‐tow digital Video Plankton Recorder for rapid surveys of plankton taxa and hydrography (2005, background): “There are many other fragile plankton that are important to quantify as well including colonial protozoa (Caron and Swanberg 1990; Dennett et al. 2002), colonial phytoplankton (e.g., Chaetoceros socialis (Sieracki et al. 1998), Rhizosolenia mats (Villareal et al. 1999), and the colo- nial…”
Real-time observation of taxa-specific plankton distributions: an optical sampling method (2004, background): “By contrast, quantification of delicate forms such as colonial radiolaria (Dennett et al. 2002), larvaceans (Benfield et al. 1996), marine snow (Ashjian et al. 2001) and algal colonies (Sieracki et al. 1998, Villareal et al. 1999) has revealed that the non-destructive nature of video sampling…”
Acquired phototrophy in aquatic protists (2009, background): “In contrast, colonial radiolarians can be abundant in the subsurface on calm days (Anderson 1983b, Dennett et al. 2002), with extreme abundances of Collozoum sp. reaching up to 20 000 colonies m–3 reported in the Gulf of Aden (Khmeleva 1967).”
Estimating zooplankton biomass through image analysis (2003, methodology): “Other methods based on image analysis, like video-recording cameras, have provided estimates of abundance and biomass of plankton organisms poorly sampled with traditional gear ( Dennett and Caron 2002 ).”
Eukaryotic plankton diversity in the sunlit ocean (2015, background): “In addition to their contribution to total primary production (36, 38), these diverse, biologically complex, often biomineralized, and relatively long-lived giant mixotrophic protists stabilize carbon in larger size fractions andprobably increase its flux to the ocean interior (38).”