Transparent exopolymer particles and dissolved organic carbon production by Emiliania huxleyi exposed to different CO2 concentrations: a mesocosm experiment
By A. Engel, B. Delille, S. Jacquet, U. Riebesell, E. Rochelle-Newall, A. Terbrüggen, I. Zondervan. 2004
199 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/4983052149055b6a938f01d4155a8c039a0d906d
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- U. Riebesell
- U. Passow
- M. Weinbauer
- Hans-Peter Grossart
- C. Carlson
- David L. Kirchman
- Hongyue Dang
- C. Robinson
In Oceanography
- U. Riebesell
- Hans-Peter Grossart
- U. Passow
- C. Robinson
- C. Carlson
- M. Weinbauer
- Jean-Pierre Gattuso
- Mark E. Warner
Citations in the corpus
- Mesocosm CO 2 perturbation studies: from organism to community level (2008, background): “– concentrations of POM and DOM (Engel et al., 2004; Rochelle-Newall et al., 2004; 10 Riebesell et al., 2007)”
- Mechanisms of Microbial Carbon Sequestration in the Ocean - Future Research Directions (2014, background): “Phytoplankton production of TEP is stimulated by higherpCO2 treatments at both species and community levels (Engel, 2002; Engel et al., 2004a; Mari, 2008; Pedrotti et al., 2012), which contributes to the formation of aggregates and so the vertical flux of POC and DOC.”
- Microbial Respiration, the Engine of Ocean Deoxygenation (2019, background): “…amount of particulate organic material (Riebesell and Tortell, 2011), a greater proportion of exudation of dissolved organic material (DOM; Engel et al., 2004) and increased carbon:nitrogen and carbon:phosphorus ratios of the DOM (Riebesell et al., 2007), leading to increased microbial…”
- Primary production during nutrient-induced blooms at elevated CO2 concentrations (2009, background): “An increasing production of TEP with increasing CO 2 concentration has previously been shown (Engel, 2002; Engel et al., 2004; Rochelle-Newall et al., 2004).”
- The biological pump in a high CO 2 world (2012, background): “Increased TEP production by phytoplankton under ocean acidification conditions has been demonstrated in one mesocosm experiment (Engel et al. 2004), but results were contradictory in another two (Schulz et al. 2008, Egge et al. 2009).”
- Acidification increases microbial polysaccharide degradation in the ocean (2009, background): “The experimental design of both mesocosm studies, however, did not allow to distinguish directpCO2- and pH-effects on bacterioplankton activity from effects induced by CO2-related changes in algal organic matter production (Engel et al., 2004; Egge et al., 2009).”
- Effect of ocean acidification on microbial diversity and on microbe-driven biogeochemistry and ecosystem functioning (2010, background): “Their results were similar to those of Engel et al. (2004) and suggested that a decrease of seawater pH would lead to a significant increase of the TEP pool.”
- Differential effects of ocean acidification on growth and photosynthesis among phylotypes of Symbiodinium (Dinophyceae) (2011, background): “…rates under OA conditions (Fu et al. 2008) and that other sinks for fixed carbon might increase in response to OA instead, such as the release of dissolved organic carbon (DOC) and production of transparent exopolymer particles (TEP), as seen in other marine phytoplankton (Engel et al. 2004, 2005).”
- Testing the effect of CO2 concentration on the dynamics of marine heterotrophic bacterioplankton (2006, background): “For example, the amount and quality of phytoplankton-derived organic matter significantly differ with pCO2 (Engel et al. 2004, 2005).”
- Effects of increased atmospheric CO 2 on small and intermediate sized osmotrophs during a nutrient induced phytoplankton bloom (2007, background): “Also, an important mechanism for15 the regulation of atmospheric CO2 concentration is the fixation of CO2 by marine phytoplankton and the subsequent export of the organically bound carbon to the deeper ocean (Engel et al., 2004).”