MORTALITY, PROTOPLASM DECAY RATE, AND RELIABILITY OF STAINING TECHNIQUES TO RECOGNIZE ‘LIVING’ FORAMINIFERA: A REVIEW
By J. Murray, S. Bowser. 2000
297 citations recorded by the source corpus.
Subfields: Atmospheric Science, Ecology
View Paper: https://www.semanticscholar.org/paper/0786dd520fc76326b35087afd6085d4ecc5b7997
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Citations in the corpus
- An illustrated guide to the benthic foraminifera of the Hebridean shelf, west of Scotland, with notes on their mode of life. (2003, background): “Therefore, live tests were easily distinguished from empty dead ones (see Murray and Bowser 2000).”
- Fidelity of variation in species composition and diversity partitioning by death assemblages: time-averaging transfers diversity from beta to alpha levels (2009, background): “…Reed 2007; Terry 2007; Zohar et al. 2008; and, as an introduction to the large live-dead literature on microbial eukaryotes and higher plants, see Hassan et al. 2008; Murray 1991; Jackson and Whitehead 1991; Jackson and Lyford 1999; Murray and Bowser 2000; Gavin et al. 2005; Zhao et al. 2006).”
- MAJOR ASPECTS OF FORAMINIFERAL VARIABILITY (STANDING CROP AND BIOMASS) ON A MONTHLY SCALE IN AN INTERTIDAL ZONE (2000, methodology): “%) is considered to be predation (Buzas and others, 1989; Murray and Bowser, 2000, and references in both).”
- TEMPORAL VARIABILITY IN VERTICAL DISTRIBUTIONS OF LIVE (STAINED) INTERTIDAL FORAMINIFERA, SOUTHERN ENGLAND (2001, methodology): “Rose Bengal is considered to be the most practical method to determine the occurrence of live specimens in this kind of study (Murray and Bowser, 2000).”
- The FOBIMO (FOraminiferal BIo-MOnitoring) initiative—Towards a standardised protocol for soft-bottom benthic foraminiferal monitoring studies (2012, background): “Furthermore, the cytoplasm of recently dead specimens degrades slowly in anoxic deeper layers, which can bias census data of rose Bengal stained specimens (Bernhard, 1988; Murray and Bowser, 2000).”
- Comparison of two methods to identify live benthic foraminifera: A test between Rose Bengal and CellTracker Green with implications for stable isotope paleoreconstructions (2006, methodology): “Rose Bengal remains the stain of choice among paleoceanographers and benthic ecologists because it is inexpensive and easy to use [ Murray and Bowser, 2000 ].”