Isolated adult populations tend to be interconnected via the larval stage. New Zealand red rock lobster Jasus edwardsii larvae metamorphose 12 to 24 mo after hatching. Because of this long larval life, J. edwardsii provides a useful species for studying population connectivity using satellite-derived ocean currents. In this study, tracks of J. edwardsii larvae originating from different populations are simulated to build a statistical picture of larval dispersal. By adding an algorithm for larval metamorphosis, and tuning the algorithm parameters to fit observed post-metamorphosis settlement patterns, we estimate where settlement in each population originated (i.e. larval sources), and also where larvae from each population settle (i.e. larval sinks). There are likely to be 4 major geographical areas for larval dispersal around New Zealand. In the far north, both sources and sinks are non-local. Along the east coast of the North Island, because of entrainment by the Wairarapa Eddy, sources are both local and distant, whereas most sinks are local. In contrast, to the south of the South Island, most sources are local, whereas sinks are both local and distant. The Chatham Islands form a separate geographical area, with primarily non-local sources and local sinks. The results are robust to differences in the physical model, but sensitive to metamorphosis algorithm parameters. This indicates that understanding larval behaviour is the most critical aspect in determining larval connectivity.KEY WORDS: Jasus edwardsii · Lobster · Larval dispersal · Numerical modelling · New Zealand · Phyllosoma · Settlement 354: 201-217, 2008 and perhaps of any benthic organism (Bradbury & Snelgrove 2001). Rock lobster larvae are known as phyllosomas (from the Greek phullon, meaning 'leaf,' and soma, meaning 'body') due to their transparent leaf-like morphology. Phyllosomas metamorphose into post-larval pueruli, which then swim shoreward to settle in the coastal zone. Pueruli have poorly developed mouth parts (Nishida et al. 1990) and apparently rely almost entirely on stored energy for their migration shoreward, implying a limit to the distance they can migrate.
Resale or republication not permitted without written consent of the publisherMar Ecol Prog SerBecause of the long larval life and limited swimming range of the pueruli, there must be some mechanism that keeps phyllosomas close enough to the coast (or brings them back) to allow them to metamorphose and then recruit successfully. Off the east coast of the North Island, phyllosomas get entrained in the Wairarapa Eddy, a semi-permanent anticyclonic eddy (Roemmich & Sutton 1998); this leads to the high levels of puerulus settlement observed south of East Cape (Booth 1994, 2002, Chiswell & Roemmich 1998. In contrast, there has been no definitive explanation of any entrainment mechanism that leads to the high settlement seen in the southwest of the South Island (part of CRA 8). It has been suggested that phyllosomas can be carried across the Tasman Sea within their lifet...