期刊
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
卷 545, 期 -, 页码 -出版社
ELSEVIER
DOI: 10.1016/j.palaeo.2020.109639
关键词
Trace fossils; Deep-sea; Contourites; Food supply; Morocco
资金
- Secretaria de Estado de I+D+I, Spain [CGL2015-66835-P]
- Junta de Andalucia [RNM-178]
- Scientific Excellence Unit (Universidad de Granada) [UCE-2016-05]
- Ministerio de Educacion, Cultura y Deporte (Gobierno de Espana)
- JIP -contourite consortium
The trace fossil Macaronichnus segregatis degiberti (7-15 mm in diameter) is recorded for the first time in deep-marine contourites which were deposited in a Late Miocene outer-shelf to upper slope of the Rifian Corridor (Morocco). Macaronichnus is typical of shallow-marine, mainly foreshore environments. It is produced by deposit feeding opheliid polychaetes in high to intermediate latitudes. This record supports the significance of bottom current processes on environmental conditions as a major limiting factor affecting the macrobenthic trace maker community. Mediterranean overflow water during the Late Miocene enabled a high nutrient supply to the seafloor, favouring colonization by Macaronichnus producers. Thus, M. s. degiberti should be used as an indicator for nutrient availability instead of mainly a palaeodepth indicator. This finding provides significant information for oceanographic and environmental reconstructions related to contouritic processes, as well as to contourite characterization.
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