Refugia for Carbonate Producing Organisms in High Carbon Dioxide Environmental Conditions

An interesting paleontological phenomenon following mass extinction events is the reappearance at a later time of a fossilizable taxon thought to have suffered extinction, but in fact survived for an extended period of time without leaving a fossil record. Several studies of larger benthic foraminifera (LBFs) that host algal symbionts have provided evidence for how some fossil taxa, sometimes referred to as "Lazarus" taxa, may have survived ocean acidification events. One study demonstrated that several species were able to live in low pH conditions in which their shells had no preservation potential. An ongoing study has demonstrated that some LBF species can tolerate much lower salinities than previously reported. The key to both observations appears to be very high carbonate alkalinity and high rates of photosynthesis. The LBFs can live and calcify under such conditions, although their shells have little or no preservation potential. Sediment samples from the Springs Coast of Florida, a region with limestone substrata and freshwater input from carbonate aquifers, were used to assess the range of Archaias angulatus, an LBF species more commonly associated with normal marine to slightly hypersaline environmental conditions found elsewhere. Extinctions of LBFs by the end of the century have been predicted due to ocean acidification, but other aspects of water chemistry, such as alkalinity influenced by the underlying substrata, may provide habitable conditions that serve as refugia until more favorable conditions return.