The life cycles of many marine species depend on a dispersive larval stage that connects
spatially segregated populations. However, quantifying larval movement among populations …

Biological dinitrogen (N 2) fixation is one mechanism by which specific microorganisms
(diazotrophs) can ameliorate nitrogen (N) limitation. Historically, rates of N 2 fixation were …

Population structure in marine teleosts is often investigated to aid conservation and fisheries
management (eg to assess population structure to inform restocking programs). We …

Suspended sediments are important contributors to the material exchanges between the sea
surface and bottom and between the coastal waters and shelf seas. The East China Sea …

The ecology of microbial assemblages inhabiting classical (positive) estuaries has been
well documented. However, we know relatively little about the microbial ecology of inverse …

Productivity is low in tropical waters outside the traditional upwelling regimes, making
temperature fronts a potential marker of fish. To test the hypothesis that all temperature fronts …

Spencer Gulf is a large (ca 22 000 km2), shallow (< 60 m water depth) embayment with
active heterozoan carbonate sedimentation. Gulf waters are metahaline (salinities 39 to …

Four water masses are identified and described using hydrographic, nutrient and stable
isotope data for the top 1000 m water depth of the southern Australian continental margin …

Many demersal marine fish species depend on a dispersive larval stage that connects
geographically discrete sub‐populations. Understanding connectivity between these sub …

Five water masses are defined for the Lincoln Shelf, South Australia using hydrographic and
stable isotope data. Three water masses are present on the shelf and slope year‐round …