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...
Main Authors: | , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Sciendo
2018-08-01
|
Series: | Geologos |
Subjects: | |
Online Access: | https://doi.org/10.2478/logos-2018-0011 |
id |
doaj-a48e3c6fb9da4785a594fd3927c55225 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT ezehsunnyc characteristictracefossilsfrommiocenebrackishwaterdepositsinthenigerdeltanigeria AT modewilfreda characteristictracefossilsfrommiocenebrackishwaterdepositsinthenigerdeltanigeria AT ozumbabertim characteristictracefossilsfrommiocenebrackishwaterdepositsinthenigerdeltanigeria |
_version_ |
1717772166193217536 |