Relationship between planktonic dinoflagellate abundance, cysts recovered in sediment traps and environmental factors in the Gullmar Fjord, Sweden

By Anna Godhe, F. Norén, M. Kuylenstierna, C. Ekberg, B. Karlson. 2001

84 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/31f4c41875ebd9955772476dd344ea6c6e76840c

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Citations in the corpus

Atlas of modern dinoflagellate cyst distribution based on 2405 data points (2013, background): “Several field studies documentmaximal cyst production during or just aftermaximal population growth when nutrients in the water column are not limited (Ishikawa and Taniguchi, 1996; Kremp and Heiskanen, 1999; Godhe et al., 2001; Sgrosso et al., 2001).”
The ups and downs of benthic ecology: considerations of scale, heterogeneity and surveillance for benthic-pelagic coupling (2003, background): “Many studies have measured the input of living material from the pelagic to the benthos using traps (Godhe et al., 2001; Hansson, 1996; Norkko et al., 2001; Whitlatch and Osman, 1998; Whitlach et al., this volume), but there have been relatively few estimates of emergence from sediments to the…”
High-resolution sediment trap study of organic-walled dinoflagellate cyst production and biogenic si (2011, result): “These values are within the range reported by other coastal sediment trap studies (Table4) (Heiskanen, 1993;Montresoret al., 1998; Godhe et al., 2001; Joyce and Pitcher, 2004; Morquecho and Lechuga-Deveze, 2004; Fujii andMatsuoka, 2006; Pitcher and Joyce, 2009; Pospelova et al., 2010).”
Spatial distribution of modern dinoflagellate cysts in polluted estuarine sediments from Buzzards Bay (Massachusetts, USA) embayments (2005, unknown): “…these mechanisms in details, one would have to tie together the studies of the motile stage of dinoflagellates in the water column, the sediment-trap studies of cyst accumulation, and simultaneous measurements of water-quality parameters (see e.g. Godhe et al. 2001) over an extended period of time.”
Major contribution of diatom resting spores to vertical flux in the sub-polar North Atlantic (2013, background): “We determined that phyto-plankton cells were responsible for generating the ﬂ ux event and that their abundance in the sediment traps varied by over 30 fold during the two-week deployment period, highlighting the ephemeral nature of downward carbon ﬂ ux during the North Atlantic spring bloom.”