TY - JOUR

T1 - Rapidly changing environmental conditions in a coastal setting during the Berriasian (“German Wealden”, lower Cretaceous): evidence from biomarker and bulk geochemical data

AU - Blumenberg, Martin

AU - Scheeder, Georg

AU - Stoepke, Fritz-Lukas Paul

AU - Pierau, Roberto

AU - Erbacher, Jochen

N1 - Publisher Copyright: © The Author(s) 2024.

PY - 2024/10/18

Y1 - 2024/10/18

N2 - During the Middle to Late Berriasian (so called “German Wealden”) a large lake system developed in the Lower Saxony Basin (LSB; in northwestern Germany) of which the eastern part is characterized by varying fluvial and lacustrine influences. The changeable situation through the earliest Cretaceous, particularly in the eastern LSB, is relatively understudied and a recently drilled well (KB-Rehburg 2; R-2) can help shedding light on these variations. R-2 covers the Berriasian ostracod zones Wealden 1 to 4 (Wd1 to Wd4), and palynomorphs presented in another study record stages with fluctuating predominantly terrigenous or aquatic organic matter. Short-term marine ingressions (MI) and more extensive transgressive events (TE) during that time interval have been reported, but some remained questionable. We here present novel organic geochemical data (including Rock–Eval and biomarkers) from R-2 showing a low maturity in terms of organic geochemical stress (Rock–Eval T max ~ 435 to 445 °C) and bulk geochemical and biomarker data support the fluctuation in the sources of the predominating organic matter. In addition to the recently published marine influx events recorded in R-2, a significant decrease in pristane/phytane and increase in dinosterane index biomarker ratios demonstrate the previously unclear TE2 at the beginning of zone Wd4. While dinoflagellate cysts during that stage were reported to occur only sporadic, the dinoflagellate-specific dinosterane biomarker became highly abundant [“dinosterane/(regular steranes + dinosteranes)” ratio up to 0.15]. It demonstrates that dinoflagellates also flourished at R-2 during zone Wd4. This palynomorph/biomarker mismatch may be explained by the prevalence of non-cyst forming, or less likely, non-preservation of cells of dinoflagellates. Our data from R-2 also points at a likely widespread and general complication for palaeoreconstructions because we observed a slight lag between first records of palynomorphs used for TE and MI event identification compared to changing biomarker ratios and bulk organic geochemistry. We hypothesize that while the first likely demonstrate first occurrences of pioneer organisms, which mark events best, organic geochemical data appear to be more integrating and record changes only after establishment of a palaeoenvironment. Graphical Abstract: (Figure presented.).

AB - During the Middle to Late Berriasian (so called “German Wealden”) a large lake system developed in the Lower Saxony Basin (LSB; in northwestern Germany) of which the eastern part is characterized by varying fluvial and lacustrine influences. The changeable situation through the earliest Cretaceous, particularly in the eastern LSB, is relatively understudied and a recently drilled well (KB-Rehburg 2; R-2) can help shedding light on these variations. R-2 covers the Berriasian ostracod zones Wealden 1 to 4 (Wd1 to Wd4), and palynomorphs presented in another study record stages with fluctuating predominantly terrigenous or aquatic organic matter. Short-term marine ingressions (MI) and more extensive transgressive events (TE) during that time interval have been reported, but some remained questionable. We here present novel organic geochemical data (including Rock–Eval and biomarkers) from R-2 showing a low maturity in terms of organic geochemical stress (Rock–Eval T max ~ 435 to 445 °C) and bulk geochemical and biomarker data support the fluctuation in the sources of the predominating organic matter. In addition to the recently published marine influx events recorded in R-2, a significant decrease in pristane/phytane and increase in dinosterane index biomarker ratios demonstrate the previously unclear TE2 at the beginning of zone Wd4. While dinoflagellate cysts during that stage were reported to occur only sporadic, the dinoflagellate-specific dinosterane biomarker became highly abundant [“dinosterane/(regular steranes + dinosteranes)” ratio up to 0.15]. It demonstrates that dinoflagellates also flourished at R-2 during zone Wd4. This palynomorph/biomarker mismatch may be explained by the prevalence of non-cyst forming, or less likely, non-preservation of cells of dinoflagellates. Our data from R-2 also points at a likely widespread and general complication for palaeoreconstructions because we observed a slight lag between first records of palynomorphs used for TE and MI event identification compared to changing biomarker ratios and bulk organic geochemistry. We hypothesize that while the first likely demonstrate first occurrences of pioneer organisms, which mark events best, organic geochemical data appear to be more integrating and record changes only after establishment of a palaeoenvironment. Graphical Abstract: (Figure presented.).

KW - Berriasian

KW - Biomarkers

KW - Bückeberg group

KW - Dinoflagellates

KW - Dinosteranes

KW - German Wealden

KW - KB-Rehburg 2 core

KW - Lower Saxony Basin (LSB)

UR - http://www.scopus.com/inward/record.url?scp=85207309432&partnerID=8YFLogxK

U2 - 10.1007/s00531-024-02470-2

DO - 10.1007/s00531-024-02470-2

M3 - Article

JO - International Journal of Earth Sciences

JF - International Journal of Earth Sciences

SN - 1437-3254

ER -