Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9522360 | Earth and Planetary Science Letters | 2005 | 12 Pages |
Abstract
The hiatuses most likely result due to the sweeping of the mound in turn with the re-establishment of vigour interglacial circulation patterns after sluggish current regimes during glacials. Thus, within the discussion if internal, fluid-driven or external environmentally driven processes control the evolution of such carbonate mounds, our findings for Propeller Mound clearly point to environmental forcing as the dominant mechanism shaping deep-water carbonate mounds in the NE Atlantic during the Late Pleistocene and Holocene.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Boris Dorschel, Dierk Hebbeln, Andres Rüggeberg, Wolf-Christian Dullo, André Freiwald,