Ml. Caplan et Rm. Bustin, Devonian-Carboniferous Hangenberg mass extinction event, widespread organic-rich mudrock and anoxia: causes and consequences, PALAEOGEO P, 148(4), 1999, pp. 187-207
The Hangenberg Bio-event represents one of the largest Phanerozoic mass ext
inction events. It is not only recorded by changes in faunal composition af
fecting all trophic levels (in the terrestrial and marine environments), bu
t is also recognized by lithological and geochemical changes just prior to
the Devonian-Carboniferous (D-C) boundary. This global faunal crisis occurs
at the base of a globally extensive black, organic-rich mudrock which shar
ply to gradationally overlies ramp and platform carbonates. Together with p
ositive excursions to the S, O, C, and Sr isotope curves, dramatic litholog
ical and faunal changes, just prior to the D-C boundary, imply an episode o
f global climatic perturbation. A low-latitude global continuum of organic
carbon generation and burial is evidenced by the formation of organic- and
phosphatic-rich black mudrocks, specific deviations to the isotope curves,
disappearance of nektobenthic organisms, diversification of small-eyed or b
lind trilobites, and the appearance of primary producers and zooplankton ac
customed to nutrient-rich conditions. It is proposed that oceanic overturn
and subsequent global eutrophication resulted in heightened primary product
ivity, the development of benthic anoxia and subsequent biotic demise of be
nthic and nektobenthic forms. Gradual climatic cooling leading to the D-C '
mini'-glaciation in Gondwana was the driving force leading to conditions of
heightened oceanic mixing and eutrophication. (C) 1999 Elsevier Science B.
V. All rights reserved.