Seasonal variation in δ13C and δ15N of size-fractionated plankton at a coastal station in the northern Baltic proper

By C. Rolff. 2000

267 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/e0a4b06370c8361c716f45630f6d75b46d62ee40

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. B. Popp
2. A. Lorrain
3. C. Hannides
4. N. Ogawa
5. N. Ohkouchi
6. Y. Chikaraishi
7. M. Landry
8. B. Graham

In Global and Planetary Change

1. B. Popp
2. C. Hannides
3. A. Lorrain
4. N. Ogawa
5. N. Ohkouchi
6. M. Landry
7. Y. Chikaraishi
8. B. Graham

In Oceanography

1. B. Popp
2. N. Ogawa
3. N. Ohkouchi
4. C. Hannides
5. Y. Chikaraishi
6. Karline Soetaert
7. Rod M. Connolly
8. M. Landry

Citations in the corpus

• Determination of aquatic food‐web structure based on compound‐specific nitrogen isotopic composition of amino acids (2009, background): “In a study conducted in the Baltic Sea, Rolff (2000) reported an annual range in δ15N values for phytoplankton of 0‰ to 7‰ and a range for zooplankton of 3‰ to 10‰.”
• The cold‐water coral community as hotspot of carbon cycling on continental margins: A food‐web analysis from Rockall Bank (northeast Atlantic) (2009, background): “The recovery depth of 800 m is much shallower than the generally accepted limit of 1500–2000 m (Rolff 2000), and thus direct decompression effects are expected to be small.”
• Small-scale spatial variability of food partitioning between cultivated oysters and associated suspension-feeding species, as revealed by stable isotopes (2007, methodology): “Polychaetes were collected with a TASM corer (40 cm core depth; Ropert & Dauvin 2000) from beneath the oyster bags.”
• Calanoid copepods feed and produce eggs in the presence of toxic cyanobacteria Nodularia spumigena (2002, background): “Decaying filaments and associated bacteria may also be consumed by ciliates and heterotrophic flagellates (Rolff 2000), which in turn can be consumed by copepods (Gifford 1991).”
• Insight into the Trophic Ecology of Yellowfin Tuna, Thunnus albacares, from Compound‐Specific Nitrogen Isotope Analysis of Proteinaceous Amino Acids (2007, background): “Unfortunately, zooplankton are also not ideal for this purpose, since they too have short life spans and many are omnivorous (Rolff 2000).”
• Feeding, reproduction and toxin accumulation by the copepods Acartia bifilosa and Eurytemora affinis in the presence of the toxic cyanobacterium Nodularia spumigena (2003, background): “Recent results suggest that cyanobacterial blooms in the Baltic Sea might play a more important role in the food web than previously assumed (Rolff 2000).”
• Reconstruction of trophic pathways between plankton and the North Iberian sardine ( Sardina pilchardus ) using stable isotopes (2004, unknown): “Some studies employed regressions of natural abundance values versus the size of organisms when grouped by size-classes (Fry and Quiñones, 1994; Rolff, 2000).”
• Stable isotope and fatty acid tracers in energy and nutrient studies of jellyfish: a review (2008, background): “Many studies have, therefore, either obtained an average signature for bulk samples of zooplankton (e.g., Malej et al., 1993), or fractionated the zooplankton by size class (e.g., obtained by sieving, Rolff, 2000 ), or used differences in densities to separate zooplankton into coarse taxonomic grou”
• Phytoplankton and macrophyte contributions to littoral food webs in the Galician upwelling estimated from stable isotopes (2006, background): “Low isotopic enrichment is expected in food webs dominated by omnivores, such as plankton systems (Fry & Quiñones 1994, Rolff 2000) while a larger fractionation is expected in more complex food webs involving specialised consumers (McClelland & Valiela 1998, Fredriksen 2003).”
• Differential δ13C and δ15N signatures among scallop tissues: implications for ecology and physiology (2002, background): “Since the early work of Stephenson et al. (1984), several authors have explored seasonal stable isotopic variation in marine organisms (Goering et al., 1990; Riera et al., 1996, Kang et al., 1999; Rolff, 2000).”
• Isotopic invisibility of protozoan trophic steps in marine food webs (2014, background): “1994), and decreased trophic complexity (fewer steps; Rolff 2000), to name a few.”
• Quantification of zooplankton trophic position in the North Pacific Subtropical Gyre using stable nitrogen isotopes (2009, background): “For example, spatial heterogeneity or seasonal cycles in N dynamics can drive significant and rapid fluctuations in d15N values at the base of the food web (Rolff 2000; Syväranta et al. 2006).”
• Efficiency of a phytoplankton‐based and a bacterial‐based food web in a pelagic marine system (2007, background): “In the Baltic Sea, the trophic distance between phytoplankton and mesozooplankton has been estimated to vary seasonally from 1.7% to 5.5% (Rolff 2000).”