Adolf Seilacher

Adolf "Dolf" Seilacher (February 24, 1925 – April 26, 2014) was a German palaeontologist who made major contributions to evolutionary and ecological palaeobiology in a career stretching over 60 years.^[1] He is best known for his contributions to the study of trace fossils; constructional morphology and structuralism; biostratinomy (including "aktuopaläontologie") exceptional preservation and the Ediacaran biota.^{[2] [3][4][5][6]}

Career

Seilacher started his career with his doctoral work under Otto Heinrich Schindewolf, professor of palaeontology at the University of Tübingen. He was also influenced by local palaeontologist Otto Linck. He served in World War II and resumed his studies at Tübingen, corresponding among others with the French ichnologist, Jacques Lessertisseur.

Gaining his doctorate in 1951 on trace fossils, Seilacher moved to the University of Frankfurt (1957) and then the University of Baghdad before taking up a chair in palaeontology in Göttingen. He returned to Tübingen in 1964 as the successor to Schindewolf. Since 1987 he has held an Adjunct Professorship at Yale University in New Haven (Connecticut), and split his time between Yale and Tübingen.

Significant work

Seilacher's publications are numerous (well over 200) and cover a range of topics. His studies on trace fossils are perhaps his best-known contributions, especially his 1967 work on the bathymetry of trace fossils. Here he established the concept of ichnofacies: distinctive assemblages of trace fossils controlled largely by depth. This characterisation was later expanded to include the influences of substrate, oxygen, salinity and so on. In addition, he analysed many trace fossils in terms of the behaviour they represent, leading to such work as early computer simulation of trace fossil morphology (with David Raup, in 1969). Much of this work is summarized together with new material in Trace Fossil Analysis (2007).

In 1970 he announced his programme of "Konstruktions-Morphologie" where he stressed the importance of three factors in determining the form of organisms: ecological/adaptive aspects; historical/phylogenetic aspects; and architectural/constructional aspects. The latter two factors are important sources of biological constraints; both acknowledging that both history and constructional principles place limits on what may be achieved in at least the short term of evolution. Such a view was influential on later workers such as Stephen Jay Gould and Richard Lewontin, such as their famous paper on "spandrels" that criticized panadaptionist accounts of evolution and form.

Seilacher's interest in pattern formation led him to espouse self-organisation models for the origin of certain types of form, the most famous of which are "pneu" structures. These are fluid-filled structures under tension whose form is broadly determined by the need to distribute the tension across the surface. Seilacher may thus be squarely considered to be a structuralist.

Seilacher has published important papers on fossil Lagerstätten, including one of 1985 that proposed a widely accepted scheme for their classification; indeed, much of his work has been concerned with preservation and taphonomy in general.

His most controversial contributions have come in his work on the Ediacaran assemblages, which he and Friedrich Pflüger (1994) suggested, based on their constructional morphology, to be pneu structures completely unrelated to modern metazoans. While this view has been steadily opposed by many workers, it has gained some ground in recent years as the affinities of many of these organisms have remained resistant to analysis. More recently, Seilacher has considered many of these taxa to be giant xenophyophores, i.e. large rhizopodal protists. He appeared in the film Volcanoes of the Deep Sea, going on a dive on the DSV Alvin to investigate modern analogues of the trace fossil Paleodictyon.

Awards

• 1983 Raymond C. Moore Medal for Paleontology ^[7]
• 1992 Crafoord Prize
• 1994 Paleontological Society Medal^[8]
• 2006 Lapworth Medal of the Palaeontological Association .^[9]

References