2nd ASEAN Symposium and Workshop on Sea Turtle Biology and Conservation. Click here

World’s first Trans-Boundary Marine Park between Sabah, Malaysia and the Philippines.

Introduction to the Turtle Island Heritage Protected Area (TIHPA)


History in the Development Of The Sabah - Philippines TIHPA


Management Objectives of the TIHPA


Institutional arrangements


Key Initiatives


Educational Goals Initiative Marked For Critical Funding


Research Objectives and Strategies


Economic Opportunities


Expected Deliverables

 

News Around the Region

Sharp decline in Turtle population


Turning to a Turtle Haven

 

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2nd ASEAN Symposium and Workshop on 
Sea Turtle Biology and Conservation

SESSION 3: Beyond the Beach....
ABSTRACTS
 

Turtles on the edge: movement of loggerhead turtles (Caretta caretta) along oceanic fronts in the central North Pacific, 1997-98

Jeffrey J. Polovina, Donald Kobayashi, Denise Ellis, Michael Seki, and George Balazs


Honolulu Laboratory, Southwest Fisheries Science Center National Marine Fisheries Service, NOAA, USA

Analyses of nine juvenile loggerheads tracked in 1997 and 1998 in the central North Pacific by satellite telemetry together with satellite remote sensed data on sea surface temperature (SST), chlorophyll, and geostrophic currents show all turtles traveling westward along two convergent oceanic fronts, against prevailing currents. These fronts are characterized by gradients in sea surface height producing an eastward geostrophic current, gradients in surface chlorophyll, and SST. Six of the turtles associated with a front characterized by 17 C SST, surface chlorophyll of about 0.2 mg/m3, and eastward geostrophic current of about 4 cm/s, while the other three turtles associated with a front with 20 C SST, surface chlorophyll of about 0.1 mg/m3, and eastward geostrophic of about 7 cm/s. These results explain why incidental catch rates of loggerheads in the Hawaii longline fishery are highest when gear is set at 17 C and 20 C SST. Further from the seasonal distribution of longline effort relative to these fronts, it appears that the surface longline fishing ground lies largely between these two fronts during the first quarter and well to the south of the 17 C front but including the 20 C front in the second quarter. Finally, these results illustrate the insights which can be achieved by combining data on movement of pelagic animals with concurrent remotely sensed environmental data.

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