J.W. Castle & J.H. Rodgers, Environ. Geosci., Hypothesis for the role of toxin-producing algae in Phanerozoic mass extinctions based on evidence from the geologic record and modern environments

Environmental Geosciences (March 2009), Vol. 16, No. 1, pp. 1-23; DOI: 10.1306/eg.08110808003
© 2009 American Association of Petroleum Geologists (AAPG)

Hypothesis for the role of toxin-producing algae in Phanerozoic mass extinctions based on evidence from the geologic record and modern environments

James W. Castle¹ and John H. Rodgers, Jr.^{2 1} Department of Environmental Engineering and Earth Sciences, Clemson University, Clemson, South Carolina 29634; jcastle@clemson.edu
² Department of Forestry and Natural Resources, Clemson University, Clemson, South Carolina 29634; jrodger@clemson.edu

Abstract

Mass mortalities of invertebrates, fish, birds, and mammals caused by algal-produced toxins are occurring in modern environments. In addition to direct effects of these toxins, the large mass of organic material produced by algal blooms can lead to oxygen depletion during decay, which indirectly causes death of some biota. Toxin-producing algae occupy a wide range of modern marine, brackish, and freshwater environments. Their growth is favored by warm water temperatures, increased inorganic carbon concentrations (e.g., CO₂), and abundant nutrient supplies in aquatic environments. Cyanobacteria (blue-green algae) are responsible for most of the disease and death caused by algal toxicity today.

Based on characteristics and occurrences of algae in modern aquatic environments and on observations from the fossil record, we propose that toxin-producing algae were present in the geologic past and were an important factor in Phanerozoic mass extinctions. The geologic record demonstrates a pronounced increase in abundance and environmental range of algae, including stromatolitic cyanobacterial mats, coincident with major Phanerozoic mass extinctions. During these past events of algal expansion, population decline of metazoan taxa could have been caused by effects of algal blooms, including algal-produced toxins, at a scale sufficient to generate a fossil record of mass extinction. Environmental changes such as climatic warming, sea level fluctuation, and increased nutrient supply may have promoted algal blooms over vast expanses of marine to freshwater environments. From the increasing frequency of modern, toxin-producing algal blooms, which may be related to global warming, another massive biotic crisis could be forthcoming.

Jim Castle is a professor at the Department of Environmental Engineering and Earth Sciences at Clemson University, where he investigates geological and environmental aspects of energy resources. He also studies modern natural and experimental systems to better understand processes relevant to past and future environmental change. He received his Ph.D. in geology from the University of Illinois.

John Rodgers received his Ph.D. from Virginia Polytechnic Institute and State University in 1977. He is currently a professor at Clemson University, the director of the Ecotoxicology Program in the Department of Forestry and Natural Resources, and the codirector of the Clemson Environmental Institute. His research involves a quest for accurate risk characterizations and development of sustainable risk mitigation tactics.

Link to abstract:  http://eg.geoscienceworld.org/cgi/content/abstract/16/1/1/