Long-eccentricity regulated climate control on fluvial incision and aggradation in the Palaeocene of north-eastern Montana (USA)

Long-eccentricity regulated climate control on fluvial incision and aggradation in the Palaeocene of north-eastern Montana (USA)

Noorbergen, Lars J. (Vrije Universiteit Amsterdam)
Turtu, Antonio (Vrije Universiteit Amsterdam)
Kuiper, Klaudia F. (Vrije Universiteit Amsterdam)
Kasse, Cornelis (Vrije Universiteit Amsterdam)
van Ginneken, Sverre (Universiteit Utrecht)
Dekkers, Mark J. (Universiteit Utrecht)
Krijgsman, Wout (Universiteit Utrecht)
Abels, H.A. (TU Delft Applied Geology)
Hilgen, Frederik J. (Universiteit Utrecht)

2020

Aggradation and fluvial incision controlled by downstream base-level changes at timescales of 10 to 500 kyr is incorporated in classic sequence stratigraphic models. However, upstream climate control on sediment supply and discharge variability causes fluvial incision and aggradation as well. Orbital forcing often regulates climate change at 10 to 500 kyr timescales while tectonic processes such as flexural (un)loading exert a dominant control at timescales longer than 500 kyr. It remains challenging to attribute fluvial incision and aggradation to upstream or downstream processes or disentangle allogenic from autogenic forcing, because time control is mostly limited in fluvial successions. The Palaeocene outcrops of the fluvial Lebo Shale Member in north-eastern Montana (Williston Basin, USA) constitute an exception. This study uses a distinctive tephra layer and two geomagnetic polarity reversals to create a 15 km long chronostratigraphic framework based on the correlation of twelve sections. Three aggradation–incision sequences are identified with durations of approximately 400 kyr, suggesting a relation with long-eccentricity. This age control further reveals that incision occurred during the approach of – or during – a 405 kyr long-eccentricity minimum. A long-term relaxation of the hydrological cycle related to such an orbital phasing potentially exerts an upstream climate control on river incision. Upstream, an expanding vegetation cover is expected because of an increasingly constant moisture supply to source areas. Entrapping by vegetation led to a significantly reduced sediment supply relative to discharge, especially at times of low evapotranspiration. Hence, high discharges resulted in incision. This study assesses the long-eccentricity regulated climate control on fluvial aggradation and incision in a new aggradation–incision sequence model.

Aggradation
climate change
fluvial stratigraphy
hiatuses
incision
long-eccentricity cycle
magnetostratigraphic correlation
tephrostratigraphic correlation

http://resolver.tudelft.nl/uuid:1a84adc7-86d4-4ee9-905c-006bd4aabe71

https://doi.org/10.1111/sed.12710

0037-0746

Sedimentology, 67 (5), 2529-2560

Institutional Repository

journal article

© 2020 Lars J. Noorbergen, Antonio Turtu, Klaudia F. Kuiper, Cornelis Kasse, Sverre van Ginneken, Mark J. Dekkers, Wout Krijgsman, H.A. Abels, Frederik J. Hilgen