Effect of somatic and otolith growth rate on stable isotopic composition of early juvenile cod (Gadus morhua L) otoliths
By H. Høie, A. Folkvord, Erling Otterlei. 2003
128 citations recorded by the source corpus.
Subfields: Ecology, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/bd0b99c5c2adae052d3cd183970c497d9feeecf5
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
In Global and Planetary Change
Citations in the corpus
- Evidence of trans-Atlantic movement and natal homing of bluefin tuna from stable isotopes in otoliths (2008, background): “…variation in δ18O between nurseries was consistent with global patterns in the oxygen isotopic ratio of seawater (LeGrande & Schmidt 2006), suggesting that otolith δ18O is closely tied to seawater δ18O for bluefin tuna and likely independent of kinetic and metabolic effects (Hoie et al. 2003).”
- Experimental evaluation of stable isotope fractionation in fish muscle and otoliths (2010, background): “Metabolic carbon contributes approximately 25% to total otolith carbon (Høie et al. 2003), but published values range between 0% (Kalish 1991) and 100% (Wurster & Patterson 2003).”
- Experimental determination of the sources of otolith carbon and associated isotopic fractionation (2006, background): “ Hoie et al. 2003 expt m Gadus morhua Measured Measured 0.28–0.32 Juvenile (< 20 mm) Aplodinotus grunniens Considered”
- Crossing the line: migratory and homing behaviors of Atlantic bluefin tuna (2014, background): “Differences in otolith δ18O values between nurseries followed an expected geographic trend in seawater δ18O (LeGrande & Schmidt 2006), which supports earlier observations that otolith δ18O is closely tied to seawater δ18O and independent of metabolic effects (Høie et al. 2003).”
- Using the δ13C and δ15N of whitefish scales for retrospective ecological studies: changes in isotope signatures during the restoration of Lake Geneva, 1980–2001 (2003, background): “Isotopic ratios of untreated and treated scales The origin of the carbonates (food or dissolved inorganic carbon) present in fish scales is not known (Hoie et al., 2003).”