scholarly journals Inter-individual variation in trophic history of Dosidicus gigas, as indicated by stable isotopes in eye lenses

2019 ◽  
Vol 4 (6) ◽  
pp. 261-267 ◽  
Author(s):  
Wei Xu ◽  
Xinjun Chen ◽  
Bilin Liu ◽  
Yong Chen ◽  
Mengyao Huan ◽  
...  
2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Fernando Gázquez ◽  
Thomas K. Bauska ◽  
Laia Comas-Bru ◽  
Bassam Ghaleb ◽  
José-María Calaforra ◽  
...  

Abstract Carbonate cave deposits (speleothems) have been used widely for paleoclimate reconstructions; however, few studies have examined the utility of other speleothem-forming minerals for this purpose. Here we demonstrate for the first time that stable isotopes (δ17O, δ18O and δD) of structurally-bound gypsum (CaSO4·2H2O) hydration water (GHW) can be used to infer paleoclimate. Specifically, we used a 63 cm-long gypsum stalactite from Sima Blanca Cave to reconstruct the climate history of SE Spain from ~ 800 BCE to ~ 800 CE. The gypsum stalactite indicates wet conditions in the cave and humid climate from ~ 200 BCE to 100 CE, at the time of the Roman Empire apogee in Hispania. From ~ 100 CE to ~ 600 CE, evaporation in the cave increased in response to regional aridification that peaked at ~ 500–600 CE, roughly coinciding with the transition between the Iberian Roman Humid Period and the Migration Period. Our record agrees with most Mediterranean and Iberian paleoclimate archives, demonstrating that stable isotopes of GHW in subaerial gypsum speleothems are a useful tool for paleoclimate reconstructions.


2018 ◽  
Vol 32 (15) ◽  
pp. 1225-1236 ◽  
Author(s):  
L.D. Trasviña-Carrillo ◽  
A. Hernández-Herrera ◽  
Y.E. Torres-Rojas ◽  
F. Galván-Magaña ◽  
A. Sánchez-González ◽  
...  

2016 ◽  
Vol 30 (13) ◽  
pp. 1461-1468 ◽  
Author(s):  
K. Rysava ◽  
R. A. R. McGill ◽  
J. Matthiopoulos ◽  
J. G. C. Hopcraft
Keyword(s):  

Author(s):  
R.I. Ruiz-Cooley ◽  
Unai Markaida ◽  
D. Gendron ◽  
S. Aguíñiga

Stomach contents and carbon (C) and nitrogen (N) stable isotope analysis were used to evaluate trophic relationships of jumbo squid, Dosidicus gigas. Buccal masses, beaks and stomach contents of large and medium maturing-sized jumbo squid and muscle from its main prey, the myctophid Benthosema panamense, were collected in the Gulf of California, Mexico during 1996, 1997 and 1999. Both the quantified C and N-isotope ratios in muscle, and stomach content analysis revealed that larger-sized maturing squid showed a higher trophic position than medium-sized individuals. However, a discrepancy between stomach contents versus stable isotope analyses was found in evaluating trophic relationships. Simple dilution models as a function of growth were used to estimate the C and N renewal dietary shift for jumbo squid. Estimates of the initial C and N pools in D. gigas with an initial age of 70 days and 210 days indicated isotopic shifts of 32% after a threefold biomass increase and 25% after a fourfold biomass increase, respectively. Additionally, beak samples of jumbo squid were evaluated as an alternative tissue to estimate squid trophic position using stable isotopes. The results showed a significant correlation between stable isotope ratios from muscle and beak samples. Muscle isotope values were higher than beak by 1% and 4% for δ13C and δ15N respectively. A test with jumbo squid beaks collected from a stomach of a stranded sperm whale confirmed the viability of this method.


2011 ◽  
Vol 356-360 ◽  
pp. 2325-2328
Author(s):  
Hai Ying Hu

The aqueous environment quality plays an important role in controlling the circulation track of ecological environment. Environmental isotopes widely exist in various kinds of water and can be extensively applied in water environment. Isotopes as natural tracers can be used to trace the transportation process of water in hydrologic cycle and the variations of isotopic value can also provide the information about the transference of contamination. The dynamical process of the movement and mix of waters can be studied by applying the composition characteristics of stable isotopes contained in natural waters, thus the main processes of water resources formation and aqueous environment evolution as well as their driving forces mechanism can be revealed. In this paper, the development history of the application of stable isotopes in the water circulation is reviewed, the application theory and analytical method of the environmental stable isotopes, and the new progress of the applied study on water resources formation and aqueous environment evolution are mainly discussed.


2020 ◽  
Vol 226 ◽  
pp. 105507
Author(s):  
Bi Lin Liu ◽  
Wei Xu ◽  
Xin Jun Chen ◽  
Meng Yao Huan ◽  
Na Liu

2011 ◽  
Vol 422 ◽  
pp. 291-302 ◽  
Author(s):  
JPY Arnould ◽  
Y Cherel ◽  
J Gibbens ◽  
JG White ◽  
CL Littnan

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