Alexandrium as a whole is wide spread across the globe and has been identified in different parts of the Northern and Southern Hemisphere. The genus can be found in oligotrophic, mesotrophic, and eutrophic coastlines. During the winter months of temperate regions, the cysts remain dormant because of the cold temperatures. They also have an internal biological clock that tells them when to germinate and thus, is the reason most of the blooms are season driven. Cysts of
A. tamarense can tolerate temperatures of −0.6 to 26.8 °C and this enables them to be well-distributed in marine seabeds. They cannot tolerate being anoxic. There may be large numbers of cyst populations, but only 20% of them can germinate and develop into a bloom, because oxygen is present mostly a few millimeters inside the sediment. Cysts have been observed to have prominent roles in genetic diversity of subpopulations and in gene flow between subpopulations. With a few exceptions, the toxic and non-toxic forms do not overlap in range because these two forms are distinct biological species that have limited sexual compatibility to other species. Scientists have observed hybrids of toxic and non-toxic forms produce lethal cells.
Alexandrium is an opportunistic dinoflagellate and thus it can bloom in nutrient-rich and nutrient-poor areas. For most species, in order for the bloom to be positively regulated it must be in a water body with high surface water temperatures, maximum water column stability, low nutrients, and low winds. In salt ponds,
Alexandrium population growth rates depend on salinity and temperature. However, in areas like the Bay of Fundy, bloom dynamics depend more readily on the mixing of tidal waters in the open region. In salt ponds,
A. fundyense migrate vertically down at night, but migrate closer to the surface of the pond during the day. However, they do not migrate too close to the surface to be flushed out with the outflowing surface water. (3) The hydro-geographical barrier and the organism's behavior restrict blooms to occur in neighbouring waters, and thus, result in high concentration of toxicity accumulating in shellfish. Other oceanographic forces include the mechanisms of upwelling winds and downwelling winds that can also play a role in bloom concentration. (10) Upwelling winds result in pushing the cells off the coast. (10) This can decline the bloom populations. However, when wind is pushing the bloom offshore, the vegetative cells can encyst and sink to the bottom of the sediment. (10) Once wind levels decrease, they transform into vegetative cells again. (3)(10) On the other hand, downwelling winds can allow the cells to be brought back to the coast and resurfaced. (10) This can have the opposite effect of localizing blooms and thereby increasing toxic concentration. (10) The time length of the blooms occur around 2–3 months. Generally, warm temperatures and sufficient nutrient concentrations can provide for excellent growth. However, even with optimal temperatures,
Alexandrium populations can be declining and this has more to do with the life cycle than what was thought to do with things like predation and parasitism. Sexuality happens well before the bloom population peaks, and a large fraction of the bloom population is mating to produce cysts that fall to the sediment. Hence, experiments have shown that temperature and nutrient availability can regulate sexuality and encystment. It has been shown that
A.catenella relies on organic nutrients produced by diatom blooms and or from picocyanobacterial. Such observations may be a reason why blooms from other protists like diatoms correlate with blooms of
Alexandrium.
Alexandrium has been increasingly more common in large city harbours, for example along the coast of the Mediterranean Sea. High
Alexandrium growth has also been typically found in low-salinity freshwater plumes. Freshwater runoffs have high organic matter, and other micronutrients, such as high iron content. Even though humans have definitely increased the amount of biomatter in the ocean, we cannot directly correlate an increase in range of
Alexandrium blooms because of human activity. This is because most blooms occur in remote and pristine waters in places like Alaska and Southern Argentina. As autotrophs,
Alexandrium species produce oxygen by consuming inorganic carbon. Organic carbon is not excreted as much compared to other phytoplankton. Inorganic carbon fixation increased or decreased either with an increase or decrease in nitrogen uptake, depending on the nutrition of the cell.
Alexandrium accumulates ammonium internally. Many species are also mixotrophs and have been observed to contain bacteria and flagellates inside food vacuoles.
A. minutum can ingest cyanobacteria.
A. catenella can ingest heterotrophic bacteria and cyanobacteria.
A. tamarense ingests haptophytes, cryptophytes, small diatoms, and
Heterosigma akashiwo.
A. tamarense has also been observed eating other dinoflagellates such as
Amphidinium carterae and
Prorocentrum minimum. Blooms can be terminated because of cell lysis, infection from viruses and/or bacteria, parasites, and encystment. Both heterotrophic and mixotrophic dinoflagellates feed on
Alexandrium. as does the ciliate
Favella.
Amoebophrya (a parasitic dinoflagellate) and
Parvilucifera (a perkinsozoan flagellate), are known to infect
Alexandrium species. Specifically,
Parvilucifer infects the mobile
zygote and pellicle cyst of
A. minutum. == Morphology and anatomy ==