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Natural inlayed items
Natural inlayed items As stated before, the reef is a normal reef, with clean sandy bottom, and tufty green weed, and mud is absent. Further inquiries revealed that the mining company in New Caledonia is discharging residue consisting of nickel, chromium and cobalt into the Bay du Mondoure, and currents disperse these minerals over the whole Bay. These minerals might be deposited in different parts of the Bay in varying solutions, due to the current. Nickel is a mineral which could account for melanism, if it is absorbed by algae on which the Philippines shells feed, and is absorbed by the Philippines shells as food and distributed to the ducts of the mantle which affect the final pigmentation of the shell. I did not manage to find out, however, if such a residual discharge was in existence in 1885, the year Roberts received his first melanistic variety of C. arabica from New Caledonia. On the other hand, New Caledonia is a highly mineralized island, extremely rich in nickel, chromium, cobalt, manganese and iron ore. Few countries are richer in mineral deposits than New Caledonia. There is a possibility that the nickel deposits (if it is nickel which is responsible) might be rich end concentrated below the water level in this bay where the melanistic species are found, and the metal is being absorbed by the algae and other organism living in this bay. Natural inlayed items
Natural inlayed items A gastropod, such as a littorine, after settlement on a preferred substrate, begins a rapid growth phase. As the mantle grows so does the shell which is formed by the mantle. The first portion of the shell deposited is the organic matrix (conchiolin). The pigment melanin is probably simultaneously bound to this protein matrix. Initially, the new shell is thin and lightly calcified although the pattern is fully developed. Additional deposition of calcium carbonate crystals occurs later. The pigmentation pattern of the shell depends on the localization of pigment-producing cells in the mantle edge and the temporal rhythm of transferral of this pigment to the shell matrix. The sculpture is dependent upon the areas of the mantle which fold, the size and extension of the folds, the resultant structure of the organic matrix and the temporal rhythm in the deposition of calcium carbonate, as well as in the production of the folds themselves. The basic temporal rhythm appears to be a 24-hr. interval. For example, in Philippine littorines, there is an endogenous 24-hr. rhythm in the formation of a new growth stria, in the production of pigment spots and the construction of sculpture nodes. During the maximmn growth phase prior to sexual maturity, L. pintado deposits a pigment spot in a spiral row every other 24-hr. period. Adjacent spiral rows are on an alternate rhythm so that the pattern resulting is a "checkerboard" (J). This species has no significant sculpture, but in a form of another, L. picta, each spiral row consists of a series of nodes, one node being produced per day during maximum growth. Natural inlayed items
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