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1 it significantly decreased their tendency to shoal.
2 wimming stickleback (Gasterosteus aculeatus) shoals.
3 ols are faster and less dense than zebrafish shoals.
4  mixing, especially if males encounter mixed shoals.
5  of time zebrafish groups spend schooling or shoaling.
6 he individual selective advantages gained by shoaling.
7 that reduced the 2-dimensional area of their shoals 15-fold compared with water-only controls.
8 ymetry and upwelling resulted in mixed-layer shoaling above the depth of minimum annual irradiance do
9 ree-dimensional structure of Antarctic krill shoals acoustically.
10 e likely to benefit from the protection of a shoal and will improve their survival chances as a resul
11  most rapidly when North Atlantic Deep Water shoaled and stratification in the Southern Ocean was red
12 ent evidence that behavioural traits such as shoaling and mate choice can promote population mixing i
13 e motion corresponding to the definitions of shoaling and schooling.
14 ystems around the unpopulated French Frigate Shoals and along the relatively lightly populated Kona C
15 ip in large, swarm-like groups, such as fish shoals and bird flocks.
16 tive behavior: birds flock, bees swarm, fish shoal, and ungulates herd.
17 roups in the wild, such as bird flocks, fish shoals, and locust swarms.
18  sea surface, many anchovies in the targeted shoal appeared to lose orientation and flowed passively
19          Tunas that will be most impacted by shoaling are Pacific and southern bluefin tunas-habitat
20 aling is adaptive, and signals that maintain shoals are likely to evolve under selection.
21 of fish can either be 'shoals' or 'schools': shoals are simply aggregations of individuals; schools a
22             Loose aggregations of fishes, or shoals, are a basal social organization of vertebrates a
23 containing massive densely populated herring shoals at night-time and diffuse herring distributions d
24       We found severe effects on feeding and shoaling behavior as well as metabolism of the fish; hen
25 study, combining the effects of mate choice, shoaling behaviour and genetics.
26 ingly, social differentiation coincided with shoals being somewhat smaller under high-perceived risk,
27                For fish, the extent to which shoaling can reduce an individual's risk of exposure to
28 levels when under stress and do not modulate shoal cohesion, indicative of abnormal social behaviour.
29 atile short-term behavior of very large fish shoals, containing tens of millions of fish and stretchi
30 largely unaffected by the early Pliocene CAS shoaling, corroborating other evidence that indicates la
31 that are highly correlated to trends in fish shoaling density and to each other over the diel cycle.
32                                 We evaluated shoal dimensions in groups of minnows exposed to O. ptyc
33 the formation processes of vast oceanic fish shoals during spawning, we show that (i) a rapid transit
34 ply aggregations of individuals; schools are shoals exhibiting polarized, synchronized motion.
35                             A model based on shoaling fish suggests how a group can show decision-mak
36 compare risk of exposure in shoaling vs. non-shoaling fish, we confined groups of minnows into mesh c
37 erences in exposure between shoaling vs. non-shoaling fish.
38 the coupling of ice and sediment dynamics: a shoal forms at the glacier terminus, reducing ice discha
39 ure given that these waters are predicted to shoal from depth over the coming decades.
40 um zones (OMZs) in midwater environments are shoaling globally; this can affect distributions of spec
41              Fish confined within artificial shoals had 3-fold fewer worms than single fish and minno
42 nows located within the centre of artificial shoals had significantly fewer worms than those without
43 strate that individuals discriminate between shoals having different pigment pattern phenotypes and t
44       We tested for antiparasite benefits of shoaling in fathead minnows exposed to larvae (cercariae
45 ata, reveal a long-term trend of thermocline shoaling in the equatorial Pacific since approximately 1
46            Overall, we project P50 depths to shoal, indicating likely habitat compression for tuna sp
47 havioral trait observed in bird flocks, fish shoals, insect swarms, and mammal herds.
48                                        Thus, shoaling is adaptive, and signals that maintain shoals a
49 nt variants demonstrate that fish can select shoal mates solely on the basis of their color patterns,
50                            Consequently, OMZ shoaling may preferentially facilitate foraging opportun
51                      The extent of isopycnal shoaling, nutricline depth, and chlorophyll concentratio
52  during which the calcite compensation depth shoaled, ocean temperatures increased and carbon isotope
53          To judge the overall direction of a shoal of fish or a crowd of people, observers must integ
54 n (Experiment 1) the dyad chose which larger shoal of guppies to join and when (Experiment 2) the dya
55 ing the last 60,000 years reflect widespread shoaling of sedimentary methane gradients and increased
56 H, thereby triggering a rapid (<10,000-year) shoaling of the calcite compensation depth (CCD), follow
57 This finding implies that the early Pliocene shoaling of the CAS had no profound impact on the evolut
58                           The early Pliocene shoaling of the Central American Seaway (CAS), ~4.7-4.2
59 ification goes together with a weakening and shoaling of the interhemispheric overturning circulation
60  reductions, weakening of the halocline, and shoaling of the intermediate-depth Atlantic Water layer
61 is linked to increased heat content and to a shoaling of the mid-depth temperature maximum over the c
62 eract anthropogenic global warming through a shoaling of the mixed layer depth (MLD) and a consequent
63     This warming is associated with a severe shoaling of the ocean calcite compensation depth and a >
64   A possible explanation is that the gradual shoaling of the oceanic thermocline reached a threshold
65 the surface shelf sediments that may lead to shoaling of the SMT.
66                                   Additional shoaling of the thermocline after 5 Myr ago probably exp
67 alf of their initial biomass, owing to rapid shoaling of winter mixed layers and their associated sep
68                                              Shoals of clupeid fish (e.g., sardine, anchovy) from geo
69          Here, we address these questions on shoals of Hemigrammus rhodostomus, a species of fish exh
70 gblenny's scope by allowing it to blend into shoals of small reef fish as well as to remain inconspic
71   For example, groups of fish can either be 'shoals' or 'schools': shoals are simply aggregations of
72 erring and krill, aggregate to form schools, shoals, or swarms (hereafter simply "schools," although
73 , female guppies did not distinguish between shoaling partners when given the choice between native a
74 n coupled with reduced availability of small shoaling pelagic fish such as sandeel (Ammodytes marinus
75  assess the impact of the early Pliocene CAS shoaling phase on deep-water circulation.
76 ges in NADW resulted from earlier and deeper shoaling phases.
77 ronmental determinants in the development of shoaling preference.
78 notypes and that early experience determines shoaling preference.
79 rience plays a key role in determining these shoaling preferences.
80 he character of which indicates that the CCD shoaled rapidly (<10,000 years) by more than 2 kilometer
81 h located within the centre of an artificial shoal reduced their risk of cercariae exposure compared
82                      These results show that shoaling reduces a minnows' risk of exposure to cercaria
83 nsively investigate the preference space for shoaling related to adult pigment pattern variation, pre
84 per direct observation, and understanding of shoaling remains incomplete.
85 posure to predation can explain the observed shoal shape.
86                                              Shoal size and packing density varied greatly, but surfa
87                         Moreover, as the OML shoals, squids will have to retreat to these shallower,
88 lability in a warming world ocean may impact shoal structure: because structure affects catchability
89 n classical experimental paradigms assessing shoaling tendency, fear, anxiety, and general locomotion
90 habituation, causing them to spend more time shoaling than schooling, contrary to most models' predic
91         Many fishes form aggregations called shoals that reduce predation risk while enhancing foragi
92 er, decreasing carbon export efficiency, and shoaling the average depths of nutrient regeneration.
93 t of the nutricline toward its western edge, shoaling the mixed layers into the base of the euphotic
94 umboldt squid are indirectly affected by OMZ shoaling through effects on a primary food source, mycto
95 oleucas) swimming in two-fish and three-fish shoals to map the mean effective forces as a function of
96               To compare risk of exposure in shoaling vs. non-shoaling fish, we confined groups of mi
97 our-mediated differences in exposure between shoaling vs. non-shoaling fish.
98  comparing data from two-fish and three-fish shoals, we challenge the standard assumption, ubiquitous
99 er region undergoing strong ocean subsurface shoaling where upper ocean heat content can drop by 20-5
100         Fish form social aggregations called shoals which often consist of fish with similar morpholo
101 pe patterning) in deciding whether to join a shoal, zebrafish female preferences do not correlate wit

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