| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441574 | Marine Geology | 2015 | 13 Pages |
Abstract
The post-transgression period witnessed the decline of mangroves, whose remnants were identified mostly in the initial 2Â m of Holocene estuarine sediments. Accelerated sea-level rise, combined with geomorphological confinement of the studied intertidal zone, was probably responsible for the demise of halophyte vegetation, which thrived again in the late Holocene.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Tomasz Boski, Fracisco H.R. Bezerra, Laura de Fátima Pereira, Anderson M. Souza, Rubson P. Maia, Francisco P. Lima-Filho,