Project A6

Seasonal and interannual variations of atmospheric circulation patterns in Eocene marginal seas of the middle latitudes

Jorit Kniest (PhD)

Principal Investigators: Jacek Raddatz, Silke Voigt, Bodo Ahrens (Goethe University Frankfurt), Bernd Schöne (University of Mainz)

The overarching objective of the VeWA subproject A6 is to gain a better understanding of the nature and development of seasonality in the mid-latitudes under a warmer climate (Eocene Greenhouse). In this context, we are particularly interested in the interaction between the atmosphere and the oceans. For this reason, we aim to find evidence of seasonal to multi-year atmospheric circulation pattern in the marine environment. In order to accomplish this aim, we will employ fossil marine bivalves as proxy archives.

Still, there is little knowledge of how the current climate change may modulate seasonal and perennial variations of atmospheric circulation pattern. Marginal seas represent a sensitive intersection between the terrestrial and marine environment, recording changes in the hydrological cycle, as variations in fresh water input. Therefore, our investigations will mainly focus on marginal seas such as, due to their fast response time to short-term climate variations. To investigate the paleo-climate conditions, we will reconstruct different environmental parameters, such as sea-surface-temperature (SST), sea-water pH and the fresh water input. To achieve this, we will utilize a variety of different geochemical proxies:

δ18O, Mg/Ca, ∆47, 48 -> Temperature

δ11B, B/Ca, δ13C, U/Ca -> pH

Ba/Ca, 87Sr/86Sr -> Terrigenous input

As proxy-archives we will use the skeletal hard parts of fossil bivalve. This taxon includes certain advantages for seasonality reconstruction. Bivalves construct their shells from separate layers, called growth increments. Each of these increment represent a certain amount of time. The time embodied within one increment can differ from a daily to annual base, depending on the species and the habitat. Sampling the particular increments generates a chronological record with a high temporal resolution, ideal for the reconstruction of seasonal oscillations.


Goethe University Frankfurt
PD. Dr. Jacek Raddatz:
Prof. Dr. Silke Voigt:
Prof. Dr. Bodo Ahrens:

Johannes Gutenberg University Mainz
Prof. Dr. Bernd Schöne: