Fish otolith chemistry influenced by exposure to multiple environmental variables

2004 ◽  
Vol 313 (2) ◽  
pp. 269-284 ◽  
Author(s):  
Travis S. Elsdon ◽  
Bronwyn M. Gillanders
2005 ◽  
Vol 56 (5) ◽  
pp. 609 ◽  
Author(s):  
T. S. Elsdon ◽  
B. M. Gillanders

Elemental concentrations within fish otoliths can track movements and migrations of fish through gradients of environmental variables. Tracking the movements of fish relies on establishing links between environmental variables and otolith chemistry, with links commonly made using laboratory experiments that rear juvenile fish. However, laboratory experiments done on juvenile fish may not accurately reflect changes in wild fish, particularly adults. We tested the hypotheses that: (1) the relationship between ambient (water) and otolith chemistry is similar between laboratory-reared black bream (Acanthopagrus butcheri) and wild black bream; and (2) ontogeny does not influence otolith chemistry. Field-collected and laboratory-reared fish showed similar effects of ambient strontium : calcium (Sr : Ca) on otolith Sr : Ca concentrations. However, ambient and otolith barium : calcium concentrations (Ba : Ca) differed slightly between laboratory-reared and field-collected fish. Importantly, fish reared in stable environmental variables showed no influence of ontogeny on Sr : Ca or Ba : Ca concentrations. Natural distributions of ambient Sr : Ca showed no clear relationship to salinity, yet, ambient Ba : Ca was inversely related to salinity. The distribution of ambient Sr : Ca and Ba : Ca in estuaries inhabited by black bream, suggest that these elements can answer different questions regarding environmental histories of fish. Reconstructing salinity histories of black bream using otolith Ba : Ca concentrations seems plausible, if adequate knowledge of Ba : Ca gradients within estuaries is obtained.


Science ◽  
1993 ◽  
Vol 260 (5106) ◽  
pp. 279-279 ◽  
Author(s):  
J. M. Kalish

Metallomics ◽  
2017 ◽  
Vol 9 (3) ◽  
pp. 239-249 ◽  
Author(s):  
Oliver R. B. Thomas ◽  
Katherine Ganio ◽  
Blaine R. Roberts ◽  
Stephen E. Swearer

2001 ◽  
Vol 58 (1) ◽  
pp. 30-38 ◽  
Author(s):  
Steven E Campana ◽  
Simon R Thorrold

The chronological properties of otoliths are unparalleled in the animal world, allowing accurate estimates of age and growth at both the daily and the yearly scale. Based on the successes of calcified structures as environmental proxies in other taxa, it was logical that researchers should attempt to link otolith biochronologies with otolith chemistry. With the benefit of hindsight, this anticipation may have been naive. For instance, the concentrations of many elements are lower in the otolith than in corals, bivalves, seal teeth, or the other bony structures of fish, making them less than ideal for elemental analyses. Nevertheless, there is growing interest in the use of otolith chemistry as a natural tag of fish stocks. Such applications are directed at questions concerning fish populations rather than using the fish as a passive recorder of the ambient environment and do not rely upon any explicit relationship between environmental variables and otolith chemistry. The questions that can be addressed with otolith chemistry are not necessarily answerable with genetic studies, suggesting that genetic and otolith studies complement rather than compete with each other. Thus, we believe that otolith applications have the potential to revolutionize our understanding of the integrity of fish populations and the management of fish stocks.


2010 ◽  
Vol 67 (4) ◽  
pp. 597-604 ◽  
Author(s):  
Karin E. Limburg ◽  
Mikael Elfman

Fish otolith chemistries are used to associate fishes with specific environments. However, otolith chemistry may also have potential as a tool in phylogenetic research, as demonstrated here in salmoniform fishes and related taxa. Two-dimensional maps of Zn:Ca otolith chemistry displayed annual oscillations in magnitude in members of the Salmoniformes (with salmons differing from whitefishes). These are also detectable in esocids, but not strongly in osmerids or in more distantly related taxa. Further, Zn:Ca magnitudes were highest in salmonids and declined in other taxa: salmonids (salmons, grayling, and whitefishes) > esocids > osmerids > other. We performed spatial analysis on sagittal section Zn:Ca maps, dividing them into five zones and obtaining means within each zone, as well as grand means. Discriminant function analysis of the different otolith zones was better able to separate taxonomic groups, but showed pike grouping more closely with salmonids and osmerids with the out-group. Zn:Ca incorporation in otoliths may be a trait under phylogenetic control, and recent re-ordering of the systematics of Salmoniformes and their sister groups may be supported by otolith Zn:Ca chemistry.


2019 ◽  
Vol 30 (1) ◽  
pp. 173-202 ◽  
Author(s):  
Jed I. Macdonald ◽  
Russell N. Drysdale ◽  
Roman Witt ◽  
Zsófia Cságoly ◽  
Guðrún Marteinsdóttir

2010 ◽  
Vol 17 (1) ◽  
pp. 17-30 ◽  
Author(s):  
Katarzyna J. Chwedorzewska

ABSTRACTThe geographic position, astronomic factors (e.g. the Earth’s maximum distance from the Sun during winter), ice cover and altitude are the main factors affecting the climate of the Antarctic, which is the coldest place on Earth. Parts of Antarctica are facing the most rapid rates of anthropogenic climate change currently seen on the planet. Climate changes are occurring throughout Antarctica, affecting three major groups of environmental variables of considerable biological significance: temperature, water, UV-B radiation.Low diversity ecosystems are expected to be more vulnerable to global changes than high diversity ecosystems


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