Uncoupling primary production from population growth in photosynthesizing organisms in aquatic ecosystems

By Z. Dubinsky, I. Berman‐Frank. Aquatic Sciences, 2001

111 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/fca4a10c0e7cff8455870adb27c18fa23a6c46fb

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. Jack J. Middelburg
2. Karline Soetaert
3. Pieter van Rijswijk
4. H. Boschker
5. Karel Van den Meersche
6. David John Suggett
7. Carlo H. R. Heip
8. S. Hennige

In Global and Planetary Change

1. Jack J. Middelburg
2. Karel Van den Meersche
3. David John Suggett
4. Pieter van Rijswijk
5. N. R. Baker
6. Karline Soetaert
7. H. Boschker
8. Mark E. Warner

In Oceanography

1. Jack J. Middelburg
2. Karline Soetaert
3. David John Suggett
4. Mark E. Warner
5. Pieter van Rijswijk
6. S. Hennige
7. Karel Van den Meersche
8. H. Boschker

Citations in the corpus

• Carbon‐nitrogen coupling and algal‐bacterial interactions during an experimental bloom: Modeling a 13C tracer experiment (2004, background): “…under nutrient-stressed conditions is caused by the preponderance of small cells with higher surface : volume ratios and, therefore, a higher capacity of passive leakage of DOC (Bjørnsen 1988), to the physiological condition of the algae (Dubinsky and Berman-Frank 2001), or a combination of both.”
• Glycogen synthesis is a required component of the nitrogen stress response in Synechococcus elongatus PCC 7942 (2013, background): “The excretion of organic carbon serves as a sink for photosynthetically produced reductant under conditions where carbon fixation rates far exceed general biomass accumulation due to limitations in available nutrients and high levels of light irradiance [1].”
• Breakdown of the coral-algae symbiosis: towards formalising a linkage between warm-water bleaching thresholds and the growth rate of the intracellular zooxanthellae (2012, unknown): “In corals exposed to elevated nutrient levels, the zooxanthellae, instead of acting like a carbon-moving conveyer belt translocating “energy” to the coral hosts, retain seven carbon atoms for every nitrogen atom absorbed from the water (Dubinsky and Berman-Frank, 2001).”
• Is photoinhibition of zooxanthellae photosynthesis the primary cause of thermal bleaching in corals? (2005, background): “A large proportion of the photosynthate produced by coral zooxanthellae is released to the host cells (Dubinsky & Jokiel, 1994; Dubinsky & Berman-Frank, 2001).”
• Photobiology of Symbiodinium revisited: bio-physical and bio-optical signatures (2009, background): “Photosynthesis by Symbiodinium produces organic matter that supplements host metabolism whilst inorganic nutrients excreted by the host in turn sustains photosynthesis (Muscatine 1990; Dubinsky and Berman-Frank 2001 ).”
• Elemental C, N, and P cell content of individual bacteria collected at the Bermuda Atlantic Time‐series Study (BATS) site (2002, result): “For balanced growth, the fluxes of N and P into new cell growth should be in equal ratios to phytoplankton C incorporation (Dubinsky and Berman-Frank 2001). Because elemental N and P incorporation is equal to the rates of photosynthetic C incorporation, we have inverted the elemental molar ratios in”
• Blooms of Baltic Sea Aphanizomenon sp. (Cyanobacteria) collapse after internal phosphorus depletion (2007, background): “Excretion of excess C is a common phenomenon among phytoplankton, and usually increases at nutrient limitation (Dubinsky & Berman-Frank 2001).”