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Movement patterns of Atlantic spotted dolphins (Stenella frontalis) and bottlenose dolphins (Tursiops truncatus) in relation to oceanographic fronts R.B. Griffin, * C. Hu +, and N.J. Griffin * * Mote Marine Laboratory + University of South Florida
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Study Area
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Atlantic spotted dolphin Stenella frontalis Bottlenose dolphin Tursiops truncatus
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Methods One-day surveys approximately 140 km in length
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Data Collected Location and abundance Digital photography for photo-identification Initial behavioral state Group follows
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Group Follows Continuous documentation of behavioral events Sequential data—3 min intervals Periodic locations of animals when in vicinity of vessel Continuous underway surface oceanography Some radio-tagging data
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S. frontalis dive data
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Sea Surface Temperature 21 Feb 2000
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Data Histogram for 19-21 March 2000 and 11-15 June 2002
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Ocean Color (Chl) 25 Jan 2002
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Underway SST: 12 April 2004 Sighting 6—S. frontalis
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Surface manifestation of thermal front
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Follow track with SST: 12 April 2004 Sighting 6—S. frontalis
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Follow track with Chl: 12 April 2004 Sighting 6—S. frontalis
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A B dLon dLat C Follow track with Chl: 12 April 2004 Sighting 6—S. frontalis
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Km/deg Lon vary as a function of cos(Lat) 1 o Lat = 111.12 km 1 o Lon = 99.01 km at 27 o Lat tan angle CBA=(AC km/BC km) arctan CBA then converted to 360 o reference A B dLon dLat C
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Tested hypothesis of uniform distribution of travel vectors, frontal vectors Tested differences in travel vectors between: 1)Possible feeding behavior 2)Season Circular statistics using Oriana (Kovach Computing Services) Rayleigh test Watson-Williams F-test Fronts and travel directions treated as axial data Tested equality of travel vectors, frontal vectors.
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Ocean Color SST S. frontalis follows
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Ocean Color SST T. truncatus follows
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November-MayJune-October S. frontalis follows
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T. truncatus follows November-MayJune-October
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Griffin and Griffin 2003, 2004 S. frontalis in highest density between 20-30 m isobaths in winter months, lowest densities in summer, while T. truncatus did not differ by season. No seasonal variation in T. truncatus movement patterns, consistent with our earlier work.
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During winter months in the eastern Gulf of Mexico, S. frontalis travels primarily in a north/south direction, in same trend as frontal location. During summer, animals travel primarily in east/west direction. Hypothesis: During winter, animals are foraging along fronts, which are better defined during this time of year. In summer, lower abundance and general east/west trend of movements suggest dolphins may be at higher densities farther from coast, with some animals making short-term foraging runs into shallower water.
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More work on frontal definition is needed. Continued group follows and photo-identification are planned to understand movement patterns and behavior of continental shelf dolphins in the eastern Gulf of Mexico.
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Harbor Branch Oceanographic Institution “Protect Wild Dolphins” Program Private donors Mote Marine Laboratory student interns
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