Biostratigraphic correlation,paleoenvironment stress,and subrosion pipe collapse: Dutch Rhaetian shales uncover their secrets |
| |
Authors: | Adiël A Klompmaker G F Waldemar Herngreen Henk W Oosterink |
| |
Institution: | (1) Department of Geology, Kent State University, 221 McGilvrey Hall, Kent, OH 44242, USA;(2) Morelissenstraat 9, 8095 PX ‘t Loo, Oldebroek, The Netherlands;(3) Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands;(4) Hortensialaan 64, 7101 XH Winterswijk, The Netherlands |
| |
Abstract: | A subrosion pipe or sinkhole is a geologic phenomenon that occurs due to dissolution of strata in the subsurface causing the
overlying sediments to collapse. The subrosion pipe in the Winterswijk quarry complex in the eastern Netherlands yielded rare,
dark-colored shales. Bivalves and palynomorphs indicate that the shales were deposited during the Rhaetian (uppermost Triassic).
In addition, detailed correlation with other NW European localities in Great Britain, Austria, and Germany further constrained
the age of the shales to the middle of the Rhaetian. The shales were deposited in a near-coastal environment and contained
a low diverse macroinvertebrate fauna with bivalves and some brittle stars that lived in a hostile environment, probably caused
by low salinity and oxygen levels. These middle Rhaetian shales were mixed with dark-colored middle to late Hettangian sediments,
both overlying Middle Triassic (Anisian) strata, which is present in the pipe as well. The presence of Rhaetian sediments
in the subrosion pipe reopened the discussion on its age of formation. We suggest that a collapse in the Middle Eocene is
most likely. This research expands the knowledge of the marine realms in the uppermost Triassic in Europe, just prior to the
Permian–Triassic extinction event. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|