Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria

Miocene deposits in the eastern portion of the Greater Ughelli, Central Swamp and Coastal Swamp depobelts contain well-developed brackish-water trace fossil assemblages. Twelve ichnogenera have been identified, namely: Asterosoma, Bergaueria, Chondrites, Gyrolithes, Thalassinoides, Lockeia, Palaeoph...

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Main Authors: Ezeh Sunny C., Mode Wilfred A., Ozumba Berti M.
Format: Article
Language:English
Published: Sciendo 2018-08-01
Series:Geologos
Subjects:
Online Access:https://doi.org/10.2478/logos-2018-0011
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spelling doaj-a48e3c6fb9da4785a594fd3927c552252021-09-06T19:22:25ZengSciendoGeologos2080-65742018-08-0124211112510.2478/logos-2018-0011logos-2018-0011Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, NigeriaEzeh Sunny C.0Mode Wilfred A.1Ozumba Berti M.2Department of Geology, University of Nigeria, Nsukka, 410001, Enugu State, NigeriaDepartment of Geology, University of Nigeria, Nsukka, 410001, Enugu State, NigeriaIndependent Petroleum Geological ConsultantMiocene deposits in the eastern portion of the Greater Ughelli, Central Swamp and Coastal Swamp depobelts contain well-developed brackish-water trace fossil assemblages. Twelve ichnogenera have been identified, namely: Asterosoma, Bergaueria, Chondrites, Gyrolithes, Thalassinoides, Lockeia, Palaeophycus, ?Conichnus, Planolites, Siphonichnus, Skolithos and Diplocraterion. In addition, common non-descript, passively filled burrows and fugichnia (escape structures) have also been observed. The above-mentioned ichnogenera and associated non-descript structures can be arranged into six distinct and recurring ichnoassociations within the Greater Ughelli, Central Swamp and Coastal Swamp depobelts. Each ichnoassociation is comprised of a group of trace fossils which collectively reflect specific environmental conditions during deposition of these Miocene strata. All trace fossil assemblages illustrate deposition in nearshore, restricted settings. Ichnological and sedimentological criteria which may be utilized to recognise brackish-water deposits are discussed and illustrated in pictures of the cores studied.https://doi.org/10.2478/logos-2018-0011ichnoassociationsichnologysalinitygreater ughellicentral swampcoastal swampneogene
collection DOAJ
language English
format Article
sources DOAJ
author Ezeh Sunny C.
Mode Wilfred A.
Ozumba Berti M.
spellingShingle Ezeh Sunny C.
Mode Wilfred A.
Ozumba Berti M.
Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria
Geologos
ichnoassociations
ichnology
salinity
greater ughelli
central swamp
coastal swamp
neogene
author_facet Ezeh Sunny C.
Mode Wilfred A.
Ozumba Berti M.
author_sort Ezeh Sunny C.
title Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria
title_short Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria
title_full Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria
title_fullStr Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria
title_full_unstemmed Characteristic trace fossils from Miocene brackish-water deposits in the Niger Delta, Nigeria
title_sort characteristic trace fossils from miocene brackish-water deposits in the niger delta, nigeria
publisher Sciendo
series Geologos
issn 2080-6574
publishDate 2018-08-01
description Miocene deposits in the eastern portion of the Greater Ughelli, Central Swamp and Coastal Swamp depobelts contain well-developed brackish-water trace fossil assemblages. Twelve ichnogenera have been identified, namely: Asterosoma, Bergaueria, Chondrites, Gyrolithes, Thalassinoides, Lockeia, Palaeophycus, ?Conichnus, Planolites, Siphonichnus, Skolithos and Diplocraterion. In addition, common non-descript, passively filled burrows and fugichnia (escape structures) have also been observed. The above-mentioned ichnogenera and associated non-descript structures can be arranged into six distinct and recurring ichnoassociations within the Greater Ughelli, Central Swamp and Coastal Swamp depobelts. Each ichnoassociation is comprised of a group of trace fossils which collectively reflect specific environmental conditions during deposition of these Miocene strata. All trace fossil assemblages illustrate deposition in nearshore, restricted settings. Ichnological and sedimentological criteria which may be utilized to recognise brackish-water deposits are discussed and illustrated in pictures of the cores studied.
topic ichnoassociations
ichnology
salinity
greater ughelli
central swamp
coastal swamp
neogene
url https://doi.org/10.2478/logos-2018-0011
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