Abstract
Skeletal carbonate mineralogy data from the literature was combined with new X-ray diffractometry data from New Zealand crabs, in order to elucidate mineralogical patterns related to body part, habitat, latitude, and phylogeny, with a view to understanding both the potential vulnerability and the preservation potential of crab shells. In general, crab carbonate is 100% Mg-calcite. In nine specimens from three New Zealand species (Austrohelice crassa, Charybdis japonica, and Hemigrapsus crenulatus) we found the first record of aragonite in brachyurid crab carbonate. Brachyurid crabs tested here generally produce Mg-calcite with mean of 6-7 wt% MgCO (sub 3) , though families Epaltidae, Majidae, Menippidae and Oziidae produ\ce high-Mg calcite (8-9 wt% MgCO (sub 3) ), while Eiphiidae and Hymenosomatidae produce low-Mg calcite (3-4 wt% MgCO (sub 3) ). Anomurid crabs showed no aragonite in any specimen, but varied more in Mg content, with the family Porcellanidae producing the highest mean Mg content found (9.3 wt% MgCO (sub 3) ). In most cases the standard deviation and range of values within species is small (SD 0-1.5, range 1-3 wt% MgCO (sub 3) . There is little evidence of partitioning of Mg in skeletal elements; Mg in the claw, for example, is not significantly different than that of the carapace, legs, or abdomen, whether considered across all species, or within individuals. Latitude (as a proxy for water temperature), too, does not appear to affect Mg in crabs, though it is possible that environment (rocky vs sandy shore) does. The strong tendency for crabs to produce mid-range Mg in calcite suggests that they may be striking a balance between mechanical strengthening of calcite while limiting solubility in sea water.