TY - DATA ID - baumann2015omat T1 - Otolith microstructure and trace elemental concentrations in juvenile Pacific bluefin tuna (Thunnus orientalis) caught off of Southern California in 2012 AU - Baumann, Hannes AU - Wells, R J D AU - Rooker, Jay R AU - Baumann, Zofia A AU - Madigan, Daniel J AU - Dewar, Heidi AU - Snodgrass, Owyn E AU - Fisher, Nicholas S PY - 2015/03/23/ T2 - Supplement to: Baumann, Hannes; Wells, R J D; Rooker, Jay R; Zhang, Saijin; Baumann, Zofia A; Madigan, Daniel J; Dewar, Heidi; Snodgrass, Owyn E; Fisher, Nicholas S (2015): Combining otolith microstructure and trace elemental analyses to infer the arrival of juvenile Pacific bluefin tuna in the California current ecosystem. ICES Journal of Marine Science, 72(7), 2128-2138, https://doi.org/10.1093/icesjms/fsv062 PB - PANGAEA DO - 10.1594/PANGAEA.844813 UR - https://doi.org/10.1594/PANGAEA.844813 N2 - We combined longitudinal analyses of otolith microstructure and trace elemental composition in ~ age 1-2 Pacific bluefin tuna (PBT, n = 24) for inferring the arrival of individuals in the California Current Large Marine Ecosystem (CCLME). Element:Ca ratios in transverse otolith sections (9-12 rows, triplicate ablations from coreprimordium to edge, ø50 µm) were quantified for eight elements: Li, Mg, Mn, Co, Cu, Zn, Sr, and Ba, which was followed by microstructure analysis to provide age estimates corresponding to each ablation spot. Age estimates from otoliths ranged from 328 to 498 days post hatch. The combined elemental signatures of four elements (Ba, Mg, Co, Cu) showed a significant increase at the otolith edge in approximately half of the individuals (30-60 days prior to catch). Given the different oceanographic properties of oligotrophic open Pacific vs. high nutrient, upwelling CCLME waters, this signal is consistent with the entry of the fish into the CCLME, which was estimated to occur primarily in July after a transoceanic migration of ~1.5-2.0 months. ER -