25 Mar 2022
25 Mar 2022
Status: this preprint is open for discussion and under review for Climate of the Past (CP).

Shallow marine carbonates as recorders of orbitally induced past climate changes – example from the Oxfordian of the Swiss Jura Mountains

André Strasser André Strasser
  • Department of Geosciences, University of Fribourg, Fribourg, 1700, Switzerland

Abstract. The detailed analysis of shallow marine carbonate sections in the Swiss Jura Mountains allows interpreting the climate changes that affected the sedimentary system during the middle to late Oxfordian (Late Jurassic). The sediments formed on a subtropical platform where carbonate-producing organisms proliferated, and ooids and oncoids were common. The sections are composed of hierarchically stacked elementary, small-scale, and medium-scale depositional sequences where facies changes imply deepening-shallowing trends. The major sequence boundaries Ox 6, Ox 7, and Ox 8 can be correlated with those of other European basins and place the studied sections in a broader framework. The chronostratigraphic tie points imply that the medium- and small-scale sequences formed in tune with the orbital eccentricity cycles of 405 and 100 kyr, respectively, and the elementary sequences with the precession cycle of 20 kyr. Orbitally controlled insolation changes at the top of the atmosphere translated into climate changes: low insolation generally resulted in low sea level amplitudes at the 20 kyr frequency, and in a cool and humid climate at the palaeolatitude of the Jura platform. Terrigenous material was eroded from the hinterland and distributed over the platform. High insolation led to sea level rise to create accommodation, and to warm and semiarid to arid conditions in which coral reefs could grow. However, nutrient input favoured growth of microbialites that encrusted the corals. The reconstruction of high-frequency sea level fluctuations based on facies analysis compares well with the curve of insolation changes calculated for the past 500 kyr. It is therefore assumed that sea level fluctuations were mainly due to thermal expansion and retraction of ocean surface water. Two models are presented that explain the formation of elementary sequences, one for low and one for high insolation. Despite the important lateral facies variations typical of a shallow marine platform, and despite the uncertainties in the reconstruction of sea level changes, this study demonstrates the potential of carbonate ecosystems to record past climate changes at a time resolution of 20’000 years. Relatively short time windows can thus be opened in the deep geologic past, and processes and products there can be compared with those of the Holocene and the Recent. For example, it appears that today’s anthropogenically induced sea level rise is more than ten times faster than the fastest rise reconstructed for the Oxfordian.

André Strasser

Status: open (until 20 May 2022)

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André Strasser

André Strasser

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Latest update: 03 Apr 2022
Short summary
Some 155 million years ago, sediments were deposited in a shallow, subtropical sea. Coral reefs formed in a warm and arid climate during high sea level, clays were washed into the ocean at low sea level and when it rained. Climate and sea level changes were induced by cyclical insolation changes. Analysing the sedimentary record, it appears that sea level rise today (as a result of global warming) is more than ten times faster than the fastest rise reconstructed from the geologic past.