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References and Notes
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the experimentally observed (R)-enantiomer
of product 4aexo. The lowest-energy cyclo-
addition transition structure displays iminium
N–H···Osulfinamide and formyl C–H···Osulfonate
hydrogen bonds (Fig. 4C), and is predicted to
have ≥1.3-kcal/mol lower energy than alterna-
tives arising from complexes II to IV, which
is consistent with the experimental data. The
basis for enantioselectivity may be ascribed
to a stabilizing p–p interaction between the
(CF3)2-C6H3N component of the catalyst and
the cationic aniline moiety of the substrate. This
interaction is evident in transition structures
leading to the major enantiomer of 4aexo (Fig.
4D), but it is absent in transition structures
leading to the minor enantiomer (Fig. 4E).
Enantioselective catalysis by 1a of a strong
Brønsted acid–catalyzed Povarov reaction thus
involves tight binding to a highly reactive cationic
intermediate through multiple, specific H-bonding
interactions, and these noncovalent interac-
tions are maintained in the subsequent stereo-
determining cycloaddition event. One of the four
energetically accessible ground-state complexes
undergoes reaction with the nucleophile prefer-
entially, illustrating the ability of bifunctional
catalyst 1a to control precisely the outcome of
this reaction through noncovalent interactions
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Supporting Online Material
Materials and Methods
SOM Text
Figs. S1 to S19
Tables S1 to S17
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5 October 2009; accepted 13 January 2010
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the Mesozoic seas have been a handful of bony
fishes confined to a brief 20-million-year window
during the Jurassic (Callovian-Tithonian, 165
to 145 million years ago) and known almost ex-
clusively from European deposits (9–12). These
enigmatic taxa belong to the extinct family
†Pachycormidae (the dagger symbol indicates
extinct groups), a stem-teleost clade that is
otherwise composed of pelagic predators con-
vergent upon tunas and billfishes (10). Giant
†pachycormids include the largest bony fish of
all time (the ~9 m †Leedsichthys) (9, 13), but
their short stratigraphic range had implied that
they were an inconsequential component of
100-Million-Year Dynasty of Giant
Planktivorous Bony Fishes in the
Mesozoic Seas
Matt Friedman,1* Kenshu Shimada,2,3 Larry D. Martin,4 Michael J. Everhart,3 Jeff Liston,5
Anthony Maltese,6 Michael Triebold6
Large-bodied suspension feeders (planktivores), which include the most massive animals to have ever
lived, are conspicuously absent from Mesozoic marine environments. The only clear representatives of
this trophic guild in the Mesozoic have been an enigmatic and apparently short-lived Jurassic group
of extinct pachycormid fishes. Here, we report several new examples of these giant bony fishes
from Asia, Europe, and North America. These fossils provide the first detailed anatomical information
on this poorly understood clade and extend its range from the lower Middle Jurassic to the end of
the Cretaceous, showing that this group persisted for more than 100 million years. Modern
large-bodied, planktivorous vertebrates diversified after the extinction of pachycormids at the
Cretaceous-Paleogene boundary, which is consistent with an opportunistic refilling of vacated ecospace.
1Department of Earth Sciences, University of Oxford, Parks
Road, Oxford OX1 3PR, UK. 2Environmental Science Program
and Department of Biological Sciences, DePaul University,
2325 North Clifton Avenue, Chicago, IL 60614, USA.
3Sternberg Museum of Natural History, Fort Hays State Uni-
versity, 3000 Sternberg Drive, Hays, KS 67601, USA. 4Natural
History Museum and Biodiversity Research Center, University
of Kansas, 1345 Jayhawk Boulevard, Lawrence, KS 66045,
USA. 5Division of Ecology and Evolutionary Biology, Faculty
of Biomedical and Life Sciences, University of Glasgow,
University Avenue, Glasgow G12 8QQ, UK. 6Triebold Paleon-
tology and Rocky Mountain Dinosaur Resource Center, 201
South Fairview Street, Woodland Park, CO 80863, USA.
he largest vertebrates—fossil or living— array of giant suspension feeders found in Ceno-
are marine suspension feeders. Modern zoic marine environments, this guild has appeared
T
clades adopting this ecological strategy to be absent during most of the Mesozoic, an
diversified in the Paleogene (66 to 23 million interval that is marked by the ecological ascend-
years ago) (1–3) and include baleen whales and ance of modern plankton groups (5, 6). Possible
four independent lineages of cartilaginous fishes candidates have been proposed (7, 8), but the
*To whom correspondence should be addressed. E-mail:
(sharks and rays) (4). In striking contrast to the clearest examples of large-bodied planktivores in mattf@earth.ox.ac.uk
990