TRACE ELEMENTS

Make your reef stand out.

  • IRON

    A cofactor enzyme, critical for photosynthesis. Iron facilitates electron transfer within zooxanthellae, supporting the production of energy and carbohydrates, via chlorophyll, for coral

  • IODIDE

    Supports coral colouration and cellular metabolic health by regulating oxidative stress, enhancing antioxidant enzyme function and contributing to immune related processes.

  • POTASSIUM

    An intracellular ion that supports zooxanthellae photosynthesis, enzyme function, and nutrient transport. In corals, it supports cellular and ionic balance enhancing pigmentation and growth.

  • FLUORIDE

    Strengthens coral skeletons by supporting aragonite stability and calcification, potentially aiding zooxanthellae efficiency, function and healthy

  • MANGANESE

    In zooxanthellae, manganese is vital for photosystem II, the light-driven process that splits water, releases oxygen, and produces energy. In corals, manganese is used for skeletal and enzymatic functions.

  • STRONTIUM

    Strontium substitutes for calcium in coral aragonite skeletons at an approximate 1:1000 ratio. This substitution stabilises the skeletal structure and facilitates calcification.

  • BROMIDE

    Supports coral and zooxanthellae health by forming sulfilimine bonds in collagen IV, aiding tissue and skeletal structures. Bromide acts synergistically with other halogens like iodine and fluorine.

  • BORON

    Supports skeletal formation by buffering pH in coral calcifying fluid, assisting aragonite precipitation. Boron may aid zooxanthellae metabolism and coral pigmentation.

  • MOLYBDENUM

    A nitrate reductase cofactor, aids zooxanthellae convert nitrate to ammonium. At 10–12 µg/L, it supports metabolism and photosynthesis, potentially reducing bleaching risk.

  • BARIUM

    Barium is a naturally occurring trace element in seawater, with concentrations ranging from 5–20 µg/L. Barium substitutes for calcium in coral skeletons at an approximate 1:100,000 ratio.

  • RUBIDIUM

    A naturally occurring trace element in seawater, with concentrations ranging from 120–200 µg/L.