2019
DOI: 10.15406/bij.2019.03.00145
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Taxonomy and phytoecology of palynomorphs and non-pollen palynomorphs: a refined compendium from the West Africa Margin

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Cited by 8 publications
(8 citation statements)
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“…The pellet deriving from the decalcification step was employed to evaluate the presence of microparticles by OM (ZEISS Axio Observer 7 equipped with polarised filters and Zen imaging software 2.6, operating at different magnifications). Starch granules, palynomorphs, NPPs, and palynodebris elements were identified on morphometric features, grouped into preliminary types based on a shared morphology, and described using conventional nomenclature 23 , 142 . Each microparticle was measured in triplicate.…”
Section: Methodsmentioning
confidence: 99%
“…The pellet deriving from the decalcification step was employed to evaluate the presence of microparticles by OM (ZEISS Axio Observer 7 equipped with polarised filters and Zen imaging software 2.6, operating at different magnifications). Starch granules, palynomorphs, NPPs, and palynodebris elements were identified on morphometric features, grouped into preliminary types based on a shared morphology, and described using conventional nomenclature 23 , 142 . Each microparticle was measured in triplicate.…”
Section: Methodsmentioning
confidence: 99%
“…The photomicrographs and microfossil taxonomical records of the three GCs published by Adojoh et al (2017Adojoh et al ( , 2019, other non-pollen proxies, and some selected key pollen/vegetation proxies are used to establish the link between vegetation dynamics and landscape evolution of the Niger Delta. The three GCs record remarkably similar changes in the different proxies and two main phases of sedimentation were distinguished (Figures 3-5).…”
Section: Resultsmentioning
confidence: 99%
“…The deltaic configuration has experienced broad progradation (circa 300 km) since the Palaeocene, with a maximum sediment thickness of approximately 12 km, and a surface area of 140,000 km 2 (Doust and Omatsola, 1990;Stacher, 1995;Reijers, 2011;George et al, 2019; Figure 2). In addition, past investigations of marine core sediments obtained from the Niger Delta suggest that changes in the riverine input during the Late Quaternary were linked to global glacial-interglacial cycles (e.g., Riboulot et al, 2012;Adojoh et al, 2017Adojoh et al, , 2019Adeonikpekun and Sowunmi, 2019). Periods of warm temperature over Greenland were found to be associated with enhanced river discharges in West Equatorial Africa and conversely, cold conditions were related to weak river input (Shannahan et al, 2007;Weldeab et al, 2007;Miller and Gosling, 2013;Adojoh et al, 2017, Adeonikpekun andSowunmi, 2019).…”
Section: Niger Delta Settingmentioning
confidence: 99%
“…Pollen/Spore species Family (Stuchlik, 2001;Adojoh et al, 2017Adojoh et al, , 2019Sciumbata et al, 2021) Botanical affinities (NLR) (Rull, 2002;Adojoh, 2017;Stuchlik, 2001;Sciumbata et al, This palynogical assembalge indicates sediment deposition in a fluvio-deltaic/nearshore environment associated with pronounced wet climatic conditions (Durugbo and Olayiwola, 2017). The occurrence of dinocysts Spiniferites trocchio et al, 2006;Guerstein et al, 2014;Mathews et al, 2018).…”
Section: No Ecological Groupmentioning
confidence: 99%