Left: Oolitic sand, mixed with a number of larger pieces of bivalve shell; the roundish ooids can be seen under magnification. Right: Live sand, which is available freshly imported or preserved in plastic bags or boxes. The basis is oolitic sand, and the rounded grains can be clearly seen when magnified. ple in Indonesia, so that trading in it has become more difficult and the product is less frequently seen on the market. LIMESTONE GRANULES By contrast, limestone granules for use as substrate are commonplace in the trade, and can also be used to fill calcium reactors. This material consists of crushed limestone deposits from fossil reefs, and is also used in horticulture—for scattering on paths in parks, for example. This substance was formerly part of living organisms—the endo- or exo-skeletons of corals, gastropods, bivalves, and sponges. The fact that it is readily available without export restrictions is a plus, but the downside is its unnatural appearance: all the grains are a similar size and have relatively sharp edges. Its precise mineral composition depends on the source; calciferous deposits originating from living organisms differ somewhat from one another, and the release of undesirable substances, such as phosphate or silicic acid, can also vary considerably. It is a good idea to test the material by putting a small sample of it in seawater and measuring the rise in phosphate or silicate using proprietary reagents. OOLITIC OR OOIDAL SAND Oolitic or ooidal sand is particularly popular in the U.S., where it comes mainly from the state of Utah. Ooids are tiny balls of limestone that originated in the sea during past geological epochs. They form in supersaturated seawater when deposits of calcium carbonate form by crystallization on tiny particles of calcium carbonate in suspension (such as grains of coral sand or bivalve shell fragments). Layer after layer is deposited until the little ball of limestone has become heavy enough to sink permanently. In earlier geological periods the resulting layers of sediment solidified into rock (oolite or oolitic limestone), and its globular components are today offered for sale in some countries as oolitic sand for use as aquarium substrate. However, ooids can also be formed from other substances, such as iron- or phosphate-based minerals, so not every ooidal sand is suitable for the marine aquarium. LIVE SAND Live sand is also now available. Originally this was mainly supplied loose and stored in aquariums in the store, but now it usually comes damp and pre-packed in breathable plastic bags. Those who advocate its use point to the fact that the material is so heavily colonized with bacteria that the newly established reef aquarium gets a boost and can be biologically loaded (livestock can be added) considerably earlier. But critics maintain that the bacterial fauna required by an aquarium cannot be preserved for long periods in a bag, but has to develop in the aquarium and will vary according to the specific organic loading. The storing of live sand for weeks or months in an aquarium—in a layer 8–12 inches (20–30 cm) thick and without any livestock—inevitably leads to the demise of the bacteria or, at the very least, a significant reduction in the bacterial population. The fact is that substrate that has been stored and transported wet releases fewer minerals of the sort that encourage algae (in particular diatoms) in the aquarium. Why is that? On the one hand, there is less erosion (by friction) of the surfaces of the grains in the transportation liquid, and because the grains are already in liquid, the mineral elements capable of being released from their surface into a liquid medium will have been released already. On the other hand, dry granulate is produced by the crushing of fossil limestone. Its surfaces are produced by the milling process and not depleted of minerals by long contact with water. That is a good thing when we want to dissolve a small amount in the calcium reactor, but disadvantageous if we want to use a large amount as substrate. In the case of coral sand, the individual components have already spent a lot of time in contact with water, so their surfaces have already become mineral-depleted, but the friction that occurs between the individual grains when the material is handled, during transportation and manual washing prior to introduction into the aquarium, will rub away the surface layer and reveal deeper layers that are not yet depleted of minerals. In some cases this can lead to more silicic acid being released, for example, and ultimately to a more serious problem with diatoms during the maturation period. So the more we rub the grains together during washing, the more mineral substances are likely to be released. In a future issue we will talk about grain size, sand bed depth, and the correct method of cleaning aquarium substrates. LEFT: J. SPRUNG; RIGHT: D. KNOP 122 CORAL
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THE REEF & MARINE AQUARIUM MAGAZINE
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EDITOR & PUBLISHER | James M. Lawre
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CORAL 5
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getting a species out of the endang
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Purchasing Marine Animals Will Neve
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Hatchery in Puerto Rico, which was
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The coelacanth Latimeria chalumnae
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of the warming of the Mediterranean
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Parenting comes at a price for male
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Inspired by Mother Nature. Engineer
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Text & images by SCOTT W. MICHAEL E
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off the coast of East Africa, east
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ONLY POLY-FILTER®AND KOLD STER-IL
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Photo courtesy of Georgia Aquarium
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eef structure. One thing to keep in
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thrIVE CORAL 33
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ILLUSTRATION: JOSHUA HIGHTER ums. F
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CORAL 37
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TK CORAL 39
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ecord of a single ornamental marine
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Seven reasons why you should use R
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WHITE & BLUE LEDS BLUE LEDS ONLY
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CORAL 47
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Size impresses humans. We marvel at
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CORAL 51
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TK I. KRAUSE CORAL 53
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Redhead Goby, Elacatinus puncticula
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TK Like mythical dwarfs, elves, and
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nonetheless a number of typical cha
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The aquarium for pygmy gobies The p
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Greenbanded Goby, Elacatinus multif
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Top left: Green Clown Goby, Gobiodo
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Candystripe Goby, Trimma cana Redfa
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69 CORAL 69
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