First published online October 21, 2004
Journal of Experimental Biology 207, 4015-4024 (2004)
Published by The Company of Biologists 2004
doi: 10.1242/jeb.01267
Tuna comparative physiology
Jeffrey B. Graham1,* and
Kathryn A. Dickson2
1 Center for Marine Biotechnology and Biomedicine and Marine Biology
Research Division, Scripps Institution of Oceanography, University of
California, San Diego, La Jolla, CA 92093-0204, USA
2 Department of Biological Science, California State University Fullerton,
Fullerton, CA 92834-6850, USA

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Fig. 2. (A) CretaceousPleistocene (CPl) time scale showing relative
cooling in benthic ocean temperature based on stable oxygen isotope ratios.
Warmest times were late Paleocene (Pa), while coolest were Pleistocene.
Numbers in circles mark the approximate timing of five major paleoceanographic
events: (1) Central American land bridge formation (3 mya); (2) beginning of
thermohaline circulation (22 mya); (3) closure of the Tethys seaway (25 mya);
(4) Antarctic glaciation and polar cooling (30 mya); (5) Northward tectonic
drift of Australia (36 mya). Data summarized from Macdougall
(1996 ); Fordyce and de Muizon
(2001 ); Graham and Dickson
(2004 ). Other Tertiary epochs
abbreviated on the left axis are: Eocene, E; Oligocene, O; Miocene, M;
Pliocene, P. (B) Phylogeny for the Sardini and Thunnini based on the earliest
known occurrences of fossil remains (orange circles) of two extant Sardini
genera (G, Gymnosarda; S, Sarda) and extant tuna genera
(A, Auxis; E/K, Euthynnus or Katsuwonus;
T, Thunnus). (Note that Thunnus fossils extend from the late
Paleocene to the Pliocene.) The extinct Paleothunnus (P) is
considered to be closely related to the tunabonito common ancestor.
Data from Bannikov (1985 );
Carroll (1988 ); Monsch
(2000 ; personal
communication). Bonito genera abbreviations: S and G, as
above; C, Cybiosarda; O, Orcynopsis. Tuna abbreviations as
in Fig. 1; the two
Thunnus subgenera (Neothunnus and Thunnus), each
with four species, are indicated. (Note: terminal lines indicate number of
extant species in each tuna genus.)
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Fig. 4. Pre-dawn to daylight acoustic track record of a South Pacific (Polynesia)
bigeye tuna, showing its deep diving in pursuit of the downward migrating deep
scattering layer (DSL). Reproduced with permission from Dagorn et al.
(2000 ).
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Fig. 7. Cladogram for Sarda and the five tuna genera (abbreviations as
above) reflecting differences in the position and the relative quantity (as
illustrated in near mid-body transverse sections) of RM (deep red), and the
phyletic trend for greater emphasis on lateral vascular supply [arteries
(red), veins (blue)] and retia (red and blue lines) for RM. See text
for detail.
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© The Company of Biologists Ltd 2004