An abrupt oceanic change and frequent climate fluctuations across the Frasnian–Famennian transition of Late Devonian: Constraints from conodont Sr isotope

Abstract

The Late Devonian Frasnian–Famennian (F‐F) transition witnessed one of the “big five” mass extinction events in the Phanerozoic. We here present high‐resolution conodont Sr isotopic data from Fuhe (South China) and Kowala (South Central Poland) sections to reveal coeval climatic and environmental variations and potential causes of this biotic crisis. Fuhe and Kowala sections yield 87Sr/86Sr ratios from 0.70815 to 0.70864 and 0.70808 to 0.70836, respectively. These Sr isotopic data demonstrate three distinctive variation cycles (I, II, and III), notably at Fuhe, fluctuating from low (negative) to higher Sr isotope ratios (positive excursion). Temporally, fluctuations I and II occurred immediately before the F‐F boundary, and fluctuation III started almost from the onset of the Famennian age. These conodont 87Sr/86Sr (low‐to‐high) fluctuations temporally match well the paces of conodont δ18O (low‐to‐high) and Δ13Ccarb‐org (high‐to‐low ) fluctuations from the identical section published previously. These Sr isotopic fluctuations thus corroborate the cyclic variations in volcanic activity/flux and weathering intensity/riverine flux in parallel with climate warm‐to‐cool fluctuations. Mass balance modelling shows the first exceptionally high Sr isotope spike (I) could have been only yielded by a dramatic increase in terrestrial flux in a somewhat restricted Palaeo‐Tethys, likely due to the closure of the oceanic domain between Laurussia and Gondwana and sea‐level fall. This scenario would enhance the seawater eutrophication/anoxia in the pericontinental basins along the Palaeo‐Tethys, causing initial strikes on the low‐latitude shallow marine benthos. Subsequently, the frequent climatic fluctuations may have further caused escalating detrimental ecological pressures, leading to their massive demise.

Phanerozoic paleotemperatures: The earth’s changing climate during the last 540 million years

“…The combined Kellwasser Extinction Event was the fourth most severe extinction event when measured in terms of ecological severity (McGhee et al, 2013). It is associated with highest sea level of the Paleozoic (Johnson, 1988;Johnson et al, 1985;Sandberg et al, 2000) as well as with a dramatic increase in 87 Sr/ 86 Sr composition of seawater (Zhang et al, 2020). For a more detailed account of the Frasnian-Famennian Extinction Event see McGhee(1996McGhee( , 2005, Racki(2005), and Sandberg(2000Sandberg( , 2002.…”

Land plant evolution and volcanism led to the Late Devonian mass extinction

“…Global biogeochemical perturbations associated with the Late Devonian extinction have been widely reported (i.e., global positive d 13 C excursions). Numerous investigations into the geologic record across the KW events revealed additional global trends which exist independent of extinction ascription, such as the precipitous decline in atmospheric CO 2 [28][29][30][31] , the rise in atmospheric O 2 to near modern levels [31][32][33][34] and the overall increase in global average temperature 35 . Given the wealth of information in the geologic record, the question arises as to whether global biogeochemical cycling supports any of these theories regarding the causal factor (or factors) driving the Late Devonian extinction.…”