Here's a couple links I thought was very interesting I came across at one point. One seems to contradict the ideal of str being mistaken for ca. (if I'm understanding that correctly) and the others touch on some other details about the biology and what might be happening. I love reading this stuff as it's nothing comparable to what's found on the forums. I wish more researchers would join the forums but I could understand why they don't!
I agree though, we've not really learned too much about why corals do what they do, but given they've been around longer than us, I'm not too quick to think I know more than the organism. I did have the thought the other day you relay, I don't believe there's any salt mixes that do not include the str/potassium/br/b/moly/etc that's been questioned so heavily as "necessary". Might be an interesting experiment though I would bet you've already seen that in the results of sps dying off after time of no supplementation...
Anyways, enjoy! Waiting for the DSR site to come back up to learn more!
However, Sr2+ and Ca2+ deposition in
G. fascicularis does not appear to involve similar biochemical mechanisms.
http://onlinelibrary.wiley.com/doi/...ionid=A8D7351290BB77630252D0D2F20F7083.f04t03
Abstract
Systematic studies on the Mg distributions, the crystal orientations, the formation mechanisms and the mechanical properties of biogenic high-Mg calcites in different marine organisms were summarized in detail in this review. The high-Mg calcites in the hard tissues of marine organisms mentioned generally own a few common features as follows. Firstly, the Mg distribution is not uniform in most of the minerals. Secondly, high-Mg calcite biominerals are usually composed of nanoparticles that own almost the same crystallographic orientations and thus they behave like single crystals or mesocrystals. Thirdly, the formation of thermodynamically unstable high-Mg calcites in marine organisms under mild conditions is affected by three key factors, that is, the formation of amorphous calcium (magnesium) carbonate precursor, the control of polymorph via biomolecules and the high Mg/Ca ratios in modern sea. Lastly, the existence of Mg ions in the Mg-containing calcite may improve the mechanical properties of biogenic minerals. Furthermore, the key progress in the synthesis of high-Mg calcites in the laboratory based on the formation mechanisms of the biogenic high-Mg calcites was reviewed. Many researchers have realized the synthesis of high-Mg calcites in the laboratory under ambient conditions with the help of intermediate amorphous phase, mixed solvents, organic/inorganic surfaces and soluble additives. Studies on the structural analysis and formation mechanisms of thermodynamically unstable biogenic high-Mg calcite minerals may shed light on the preparation of functional materials with enhanced mechanical properties.
http://www.sciencedirect.com/science/article/pii/S1047847713003031
The development of chemical routes leading to controlled crystallization is an important requirement in the synthesis of crystalline materials for various applications. New synthetic approaches are often inspired by biology, which shows countless examples of biogenic crystals with finely tuned sizes, shapes, crystallographic orientation, polymorphs, etc.1 In particular, the importance of calcium carbonates in nature has led to extensive studies of CaCO3 crystallization using two main bioinspired methods: (i) templating by structured organic surfaces,2-4 such as self-assembled monolayers (SAMs), Langmuir monolayers, biomacromolecules, and functionalized polymers; and (ii) solution precipitation with growth modifiers,5-8 such as ions, proteins, and synthetic polymers.
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In summary, we have demonstrated the highly controlled synthesis of calcite with uniform nucleating plane, size, and morphology, by combining the MUA-SAM-induced oriented nucleation with the addition of Mg2+ ions to the growth solution. The ability to form a statistically significant number of homogeneous crystals makes this approach suitable for detailed studies of the mechanisms of the oriented nucleation and of the incorporation of the impurities into the crystals. We suggest, therefore, that the use of the templating by chemically modified surfaces together with specialized growth modifiers in the crystallizing solution is a promising chemical route to yield high-level control of multiple parameters of crystallization in one experiment, including crystal orientation, size, shape, polymorph, and stability.
http://aizenberglab.seas.harvard.edu/files/2003_JACS_0.pdf