Climatic fluctuations and seasonality during the Kimmeridgian (Late Jurassic)

Stable isotope and clay mineralogical data from the Lower Saxony Basin, Northern Germany

verfasst von

Fanfan Zuo, Ulrich Heimhofer, Stefan Huck, Thierry Adatte, Jochen Erbacher, Stéphane Bodin

Abstract

In previous palaeoclimatic models, the Kimmeridgian stage has been defined as a typical greenhouse-time interval with weak latitudinal gradients. However, palaeoclimatic information based on biogenic low-Mg calcite δ¹⁸O for the Kimmeridgian is still limited. Here, shell materials (n = 81) precipitated by brachiopods, oysters and Trichites bivalves from the Lower Saxony Basin, Northern Germany are evaluated for their potential to act as archive for marine sea-surface temperatures. Furthermore, the associated clay mineral assemblages based on bulk materials are used to infer hinterland weathering patterns and overall climatic conditions simultaneously. The established sea-surface temperature curve reveals an overall slightly warming trend through the Kimmeridgian. Weak seasonality (~4 °C) in sea-surface temperatures is documented by oxygen isotope variations measured along the growth lines of a large Trichites shell. Distinctly higher δ¹⁸O values observed in the Lower Kimmeridgian (late Baylei Chron) are interpreted to be related to the short-term influx of cooler boreal water masses. Judging from the corresponding smectite-dominated interval, however, the positive oxygen isotope anomaly may also be partly explained by a relatively drier climate causing enhanced δ¹⁸O_seawater values due to intensified evaporation. The kaolinite/(illite + chlorite) ratio points to a slightly long-term decrease in humidity through the Kimmeridgian on the landmasses surrounding the LSB. The short-term fluctuations in humid/arid conditions correlate significantly with sea-level changes, with humid climates accompanying high sea-levels and arid climates accompanying low sea-levels. Results from this study provide new insights into Late Jurassic climatic dynamics and help to establish a reliable Subboreal Late Jurassic sea-surface temperature curve.

Organisationseinheit(en)

Leibniz Forschungszentrum FZ:GEO
Institut für Geologie
Abteilung Geologie
AG Sedimentologie, Stratigraphie und Palynologie

Externe Organisation(en)

Université de Lausanne (UNIL)
Landesamt für Bergbau, Energie und Geologie (LBEG)
Aarhus University

Typ

Artikel

Journal

Palaeogeography, Palaeoclimatology, Palaeoecology

Band

517

Seiten

1-15

Anzahl der Seiten

15

ISSN

0031-0182

Publikationsdatum

01.03.2019

Publikationsstatus

Veröffentlicht

Peer-reviewed

Ja

ASJC Scopus Sachgebiete

Ozeanographie, Ökologie, Evolution, Verhaltenswissenschaften und Systematik, Erdoberflächenprozesse, Paläontologie

Ziele für nachhaltige Entwicklung

SDG 13 – Klimaschutzmaßnahmen, SDG 14 – Lebensraum Wasser

Elektronische Version(en)

https://doi.org/10.1016/j.palaeo.2018.12.018 (Zugang: Geschlossen)