Abstract:Periodic increments within the squid statolith microstructure are now routinely used to obtain individual age estimates. Validation and culture studies have shown that statolith increments (similar to increments in larval fish otoliths) are produced daily in a number of squid species and in one sepioid. However, sample sizes for validation studies are small and there is need for further, more comprehensive validation experiments. Statolith age analysis has revealed that temperate squids can complete their life… Show more
“…Both structures are composed primarily of calcium carbonate and are formed of alternating layers of protein and aragonite that are deposited on a daily basis (Jackson 1994). The chemistry of fish otoliths has been used extensively to reconstruct environmental histories of individuals and as natural tags of stock structure (Campana 1999).…”
Section: Discussionmentioning
confidence: 99%
“…Squid statoliths are composed primarily of aragonite crystals associated with an organic matrix (Radtke 1983). Alternating layers of protein-rich and organic-poor material are deposited on a daily basis in squid statoliths (Jackson 1994). The presence of validated daily increments confirms that material is deposited in statoliths throughout the life of the squid and provides a method for accurate age estimation of individuals.…”
Section: Introductionmentioning
confidence: 87%
“…Daily deposition of statolith growth increments has been validated in a number of loliginid species both in captivity (Jackson 1994) and in the wild (Lipinski et al 1998). Statolith microstructure in L. gahi was similar to that of other loliginids, so we assumed that the growth increments within L. gahi statoliths were deposited daily and that the total number of increments in a statolith represented the postembryonic age of squid in days.…”
Abstract:We quantified elemental signatures in statoliths of 718 Patagonian longfin squid (Loligo gahi) collected in the vicinity of the Falkland Islands (southwest Atlantic) and at sites on the Patagonian Shelf and coastal Peru. All squid were assigned to a spawning cohort by size, spawning condition, and back-calculated spawning date based on daily increments in statoliths. The remaining statolith was then analyzed for six elemental ratios (Mg/Ca, Mn/Ca, Sr/Ca, Cd/Ca, Ba/Ca, and Pb/Ca) using high-resolution inductively coupled plasma mass spectrometry (ICP-MS). Elemental concentrations in the statoliths were broadly similar to other biogenic aragonites. Differences in Sr/Ca ratios in statoliths among geographic locations were generally consistent with a negative correlation between Sr/Ca and temperature. Variations in statolith Cd/Ca and Ba/Ca values confirmed that during winter months, the squid were foraging deeper in the water column. Both Mg/Ca and Mn/Ca ratios in statoliths decreased with squid size, probably corresponding to a decrease in the contribution of the organic component of the statolith. Elemental signatures in the statoliths of L. gahi varied significantly geographically and between spring-and autumn-spawned cohorts, which must therefore have spent significant portions of their life histories in different environments.
Résumé : Nous avons quantifié les signatures d'éléments dans les statolithes de 718 calmars patagons (Loligo gahi)récoltés dans les environs des îles Falkland (Atlantique sud) et à certains sites sur la plate-forme patagonienne et la côte du Pérou. Tous les calmars ont été assignés à une cohorte de fraye d'après leur taille, leur état reproductif et leur date de fraye déterminée par rétrocalcul à partir des couches de croissance journalière sur les statolithes. Nous avons déterminé six rapports d'éléments dans le second statolithe, soit Mg/Ca, Mn/Ca, Sr/Ca, Cd/Ca, Ba/Ca et Pb/Ca, après une analyse par spectrométrie de masse à source de plasma à couplage inductif (ICP-MS) de haute résolution. Les concentrations d'éléments dans les statolithes sont grossièrement semblables à celles des autres aragonites d'origine biologique. Les différences de Sr/Ca dans les statolithes provenant des diverses localités géographiques s'accordent en général avec la corrélation négative qui existe entre Sr/Ca et la température. Les variations de Cd/Ca et de Ba/Ca dans les statolithes confirment que durant les mois d'hiver les calmars recherchent leur nourriture à de plus grandes profondeurs dans la colonne d'eau. Les rapports Mg/Ca et Mn/Ca déclinent tous les deux à mesure que le calmar grandit, ce qui correspond probablement à une diminution de la contribution de la composante organique du statolithe. Les signatures des éléments des statolithes de L. gahi varient de façon significative en fonction du site géographique, ainsi qu'entre les cohortes pondues au printemps et à l'automne, qui doivent alors avoir passé une partie significative de leur temps dans des environnements différents.[Traduit par l...
“…Both structures are composed primarily of calcium carbonate and are formed of alternating layers of protein and aragonite that are deposited on a daily basis (Jackson 1994). The chemistry of fish otoliths has been used extensively to reconstruct environmental histories of individuals and as natural tags of stock structure (Campana 1999).…”
Section: Discussionmentioning
confidence: 99%
“…Squid statoliths are composed primarily of aragonite crystals associated with an organic matrix (Radtke 1983). Alternating layers of protein-rich and organic-poor material are deposited on a daily basis in squid statoliths (Jackson 1994). The presence of validated daily increments confirms that material is deposited in statoliths throughout the life of the squid and provides a method for accurate age estimation of individuals.…”
Section: Introductionmentioning
confidence: 87%
“…Daily deposition of statolith growth increments has been validated in a number of loliginid species both in captivity (Jackson 1994) and in the wild (Lipinski et al 1998). Statolith microstructure in L. gahi was similar to that of other loliginids, so we assumed that the growth increments within L. gahi statoliths were deposited daily and that the total number of increments in a statolith represented the postembryonic age of squid in days.…”
Abstract:We quantified elemental signatures in statoliths of 718 Patagonian longfin squid (Loligo gahi) collected in the vicinity of the Falkland Islands (southwest Atlantic) and at sites on the Patagonian Shelf and coastal Peru. All squid were assigned to a spawning cohort by size, spawning condition, and back-calculated spawning date based on daily increments in statoliths. The remaining statolith was then analyzed for six elemental ratios (Mg/Ca, Mn/Ca, Sr/Ca, Cd/Ca, Ba/Ca, and Pb/Ca) using high-resolution inductively coupled plasma mass spectrometry (ICP-MS). Elemental concentrations in the statoliths were broadly similar to other biogenic aragonites. Differences in Sr/Ca ratios in statoliths among geographic locations were generally consistent with a negative correlation between Sr/Ca and temperature. Variations in statolith Cd/Ca and Ba/Ca values confirmed that during winter months, the squid were foraging deeper in the water column. Both Mg/Ca and Mn/Ca ratios in statoliths decreased with squid size, probably corresponding to a decrease in the contribution of the organic component of the statolith. Elemental signatures in the statoliths of L. gahi varied significantly geographically and between spring-and autumn-spawned cohorts, which must therefore have spent significant portions of their life histories in different environments.
Résumé : Nous avons quantifié les signatures d'éléments dans les statolithes de 718 calmars patagons (Loligo gahi)récoltés dans les environs des îles Falkland (Atlantique sud) et à certains sites sur la plate-forme patagonienne et la côte du Pérou. Tous les calmars ont été assignés à une cohorte de fraye d'après leur taille, leur état reproductif et leur date de fraye déterminée par rétrocalcul à partir des couches de croissance journalière sur les statolithes. Nous avons déterminé six rapports d'éléments dans le second statolithe, soit Mg/Ca, Mn/Ca, Sr/Ca, Cd/Ca, Ba/Ca et Pb/Ca, après une analyse par spectrométrie de masse à source de plasma à couplage inductif (ICP-MS) de haute résolution. Les concentrations d'éléments dans les statolithes sont grossièrement semblables à celles des autres aragonites d'origine biologique. Les différences de Sr/Ca dans les statolithes provenant des diverses localités géographiques s'accordent en général avec la corrélation négative qui existe entre Sr/Ca et la température. Les variations de Cd/Ca et de Ba/Ca dans les statolithes confirment que durant les mois d'hiver les calmars recherchent leur nourriture à de plus grandes profondeurs dans la colonne d'eau. Les rapports Mg/Ca et Mn/Ca déclinent tous les deux à mesure que le calmar grandit, ce qui correspond probablement à une diminution de la contribution de la composante organique du statolithe. Les signatures des éléments des statolithes de L. gahi varient de façon significative en fonction du site géographique, ainsi qu'entre les cohortes pondues au printemps et à l'automne, qui doivent alors avoir passé une partie significative de leur temps dans des environnements différents.[Traduit par l...
“…Both structures are composed of calcium carbonate and high molecular proteins. Visible increments are formed of alternating layers of protein and aragonite (Clarke 1978;Kristensen 1980;Jackson 1994). These growth rings are frequently used for age determination since a daily deposition of increments has been validated for several cephalopod species including Sepia officinalis (Bettencourt and Guerra 2001).…”
The use of statolith chemistry to trace migration pathways and distinguish populations of cephalopods is based on the assumption that the elemental composition of statoliths is influenced by physicochemical properties of the ambient environment. However, such influences have not been investigated experimentally up until now. This study presents the first microchemical analyses of cephalopod statoliths obtained from laboratory experiments under different controlled temperature and salinity conditions. Our results show that statolith chemical composition is strongly related to both salinity and temperature in ambient waters. The Ba/Ca ratio is negatively related to temperature and shows no relation to salinity. The I/Ca ratio is positively related to temperature and negatively to salinity. No Sr/Ca relation was found to either salinity or temperature, suggesting that the well-established proxy strontium is not as useful in cephalopod statoliths as in other biomineralized aragonites. Microanalysis of trace elements, however, shows an enormous potential for field studies on distribution, migration and stock separation of cephalopods. Furthermore, Synchrotron X-ray Fluorescence Analysis is introduced as a promising novel method for statolith analysis, providing a spatial resolution of typically 10-15 lm combined with detection limits down to 0.5 ppm.
“…statoliths, spines), can provide a permanent record of traits such as size, age, and growth (e.g. Campana & Neilson 1985, Jackson 1994). This feature makes it possible to measure selective mortality in the absence of information about individual fates.…”
Selective mortality is an important process influencing both the dynamics of marine populations and the evolution of their life histories. Despite a large and growing interest in measuring selective mortality, studies of marine species can face some serious methodological and analytical challenges. In particular, many studies of selection in marine environments use a crosssectional approach in which fates of individuals are unknown but the distributions of trait values before and after a period of selective mortality may be compared. This approach is often used because many marine species have morphological structures (e.g. otoliths in fishes, statoliths in some invertebrates) that contain a permanent record of trait values. Although these structures often contain information on multiple, related traits, interpretation of selection measures has been limited because most studies of selection based on cross-sectional data consider selection 1 trait at a time, despite known problems with trait correlations. Here, we detail how cross-sectional data can be analyzed within a multivariate framework and provide a practical guide for conducting these types of analyses. We illustrate these methods by applying them to empirical studies of selective mortality on early life history traits in 2 species of reef fish. These examples demonstrate that analyzing selective mortality in a multivariate framework can vastly improve estimates of selection and yield new insight into how combinations of traits can interact to influence survival. Accompanying the paper are 2 R scripts that can be used to perform the calculations described here and assist with visualizing selection on multiple traits.
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