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Journal articles on the topic 'Cameroon Line'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Déruelle, Bernard, Jean N'ni, and Robert Kambou. "Mount Cameroon: an active volcano of the Cameroon Line." Journal of African Earth Sciences (1983) 6, no. 2 (1987): 197–214. http://dx.doi.org/10.1016/0899-5362(87)90061-3.

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2

Nemzoue, P. N. N., N. A. K. Keutchafo, and J. P. Tchouankoue. "GEOTHERMAL DEVELOPMENT IN CAMEROON." Revista de Engenharia Térmica 19, no. 1 (2020): 32. http://dx.doi.org/10.5380/reterm.v19i1.76428.

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Africa is currently experiencing a period of economic growth. Its population is growing rapidly and its economies grow and diversify. To be sustainable, such growth requires a large investment in the energy sector. In the case of Cameroon hydroelectric energy is the main source of electrical power whereas the analysis of the geological point of view shows that Cameroon is unique in west-northern of Africa for its active volcanic line (with the last eruption of Mount Cameroon that last erupted in 1999 and 2000) that is a favorable zone for the production of power from geothermal resources. The

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3

Barfod, D. N. "Noble Gases in the Cameroon Line." Mineralogical Magazine 62A, no. 1 (1998): 118–19. http://dx.doi.org/10.1180/minmag.1998.62a.1.62.

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4

Gonmadje, Christelle, Charles Doumenge, Terry Sunderland, Michael Balinga, and Bonaventure Sonké. "Analyse phytogéographique des forêts d'Afrique Centrale: le cas du massif de Ngovayang (Cameroun)." Plant Ecology and Evolution 145, no. (2) (2012): 152–64. https://doi.org/10.5091/plecevo.2012.573.

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Phytogeographical analysis of Central African forests: the Ngovayang massif (Cameroon) <b>Background and aims</b> – The Ngovayang massif, in southern Cameroon, is part of a group of small hills along the Atlantic coast of the Gulf of Guinea. This area is known for its floristic richness and its high level of endemism. We conducted a phytogeographical analysis of this massif and evaluated its floristic affinities with other forested sites in Central Africa. <b>Methods</b> – Phytogeographical analysis was based on a comparison of lists of tree species with dbh ≥ 10 cm, inventoried in 1-ha perman

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5

Tanjong, Ashuntantang Tobias. "When Harmonization Crosses the Red Line: Interrogating the Post-1972 Common Law Ethnocide in Anglophone Cameroon." International Journal of Research and Innovation in Social Science VII, no. X (2023): 2218–32. http://dx.doi.org/10.47772/ijriss.2023.701169.

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By dint of their disparate colonial groomings, Anglophone Cameroon had common law as its legal system at the dawn of reunification in 1961 while Francophone Cameroon had civil law. Things would stay that way until 1972 when the government began sanctifying civil Law over common law through an asymmetric and assimilatory harmonization scheme. That was the beginning of the systematic erosion of common law in Anglophone Cameroon and the contemporaneous transposition of civil law to the territory. Anglophone common law practitioners manifested their revulsion to this harmonization travesty through

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6

Tanyileke, G. Z., M. Kusakabe, and W. C. Evans. "Chemical and isotopic characteristics of fluids along the Cameroon Volcanic Line, Cameroon." Journal of African Earth Sciences 22, no. 4 (1996): 433–41. http://dx.doi.org/10.1016/0899-5362(96)00025-5.

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7

Kochemasov, G. G. "The Cameroon line: its regularities and relation to African rifts." Global Tectonics and Metallogeny 9 (January 1, 2007): 67–72. http://dx.doi.org/10.1127/gtm/9/2007/67.

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8

Ubangoh, R. U., I. G. Pacca, J. B. Nyobe, J. Hell, and B. Ateba. "Petromagnetic characteristics of Cameroon Line volcanic rocks." Journal of Volcanology and Geothermal Research 142, no. 3-4 (2005): 225–41. http://dx.doi.org/10.1016/j.jvolgeores.2004.11.006.

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9

Hlaváč, Peter, Petr Baňař, and Eric Bertrand Fokam. "Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon." Zootaxa 5323, no. 2 (2023): 255–67. https://doi.org/10.11646/zootaxa.5323.2.5.

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Hlaváč, Peter, Baňař, Petr, Fokam, Eric Bertrand (2023): Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon. Zootaxa 5323 (2): 255-267, DOI: 10.11646/zootaxa.5323.2.5, URL: http://dx.doi.org/10.11646/zootaxa.5323.2.5

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10

Nkouathio, D. G., J. J. Ménard, P. Wandji, and J. M. Bardintzeff. "The Tombel graben (West Cameroon): a recent monogenetic volcanic field of the Cameroon Line." Journal of African Earth Sciences 35, no. 2 (2002): 285–300. http://dx.doi.org/10.1016/s0899-5362(02)00031-3.

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11

Ngounouno Yamgouot, Fadimatou, Isaac Bertrand Gbambie Mbowou, Ismaïla Ngounouno, Azizi Abdoul Youpoungam, Isaac Daama, and Bernard Déruelle. "Insight into geochemistry of basaltic rocks from Mt Cameroon and characterization of the mantle source." International Journal of Advanced Geosciences 6, no. 2 (2018): 151. http://dx.doi.org/10.14419/ijag.v6i1.10738.

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Alkaline volcanic activities occurred in the Mt Cameroon at the ocean-continent boundary of the Cameroon Line. It is characterized by a volcanic association of alkali basalts and hawaiites extruded during the late Miocene to Recent times. The major and trace element geochemistry of the Mt Cameroon are consistent with the fractional crystallization of olivine ± clinopyroxene ± plagioclase (± amphibole). Petrographical and mineralogical study reveals the presence of xenocryts (olivine, clinopyroxene and spinel) in Mt Cameroon basalts. Their composition are similar to xenoliths and rocks crystals

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12

Tabod, C. T., J. D. Fairhead, G. W. Stuart, B. Ateba, and N. Ntepe. "Seismicity of the Cameroon Volcanic Line, 1982–1990." Tectonophysics 212, no. 3-4 (1992): 303–20. http://dx.doi.org/10.1016/0040-1951(92)90297-j.

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13

Sztucki, Jerzy. "Case Analysis: Case Concerning Land and Maritime Boundary (Cameroon v. Nigeria): Provisional Measures, Order of 15 March 1996." Leiden Journal of International Law 10, no. 2 (1997): 341–58. http://dx.doi.org/10.1017/s0922156597000290.

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By an application filed on 29 March 1994, Cameroon instituted proceedings against Nigeria, relying on the declarations under Article 36(2) of the Statute of the Court, made by both states without reservations. The dispute, according to the Application, related “essentially to the question of sovereignty over the Bakassi Peninsula”, where, “since the end of 1993”, the Nigerian troops were “occupying several Cameroonian localities”. Cameroon also requested the Court “to determine the course of the maritime boundary between the two states beyond the line fixed in 1975”. In an ‘Additional Applicat

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14

Mouzong, Marcelin Pemi, Inoussah Moungnutou Mfetoum, Simon Koumi Ngoh, Prosper Gopdjim Noumo, and Jean Gaston Tamba. "Current Status, Future Prospects, and the Need for Geothermal Energy Exploration in Cameroon: Comprehensive Review." Geofluids 2023 (August 24, 2023): 1–13. http://dx.doi.org/10.1155/2023/6168519.

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Cameroon is a country in Central Africa that relies heavily on hydropower, fossil fuels, solar, and biomass for its energy needs. However, the unstable and intermittent nature of these energy sources makes them unreliable, and there is a pressing need for a more secure and sustainable energy supply. Geothermal energy, which is abundant in Cameroon due to its favorable geological characteristics, has not been fully explored as a potential energy source. This study is aimed at providing a comprehensive review of the current status and future prospects of geothermal energy in Cameroon, based on p

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15

Burke, Kevin. "Origin of the Cameroon Line of Volcano‐Capped Swells." Journal of Geology 109, no. 3 (2001): 349–62. http://dx.doi.org/10.1086/319977.

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16

Milelli, L., L. Fourel, and C. Jaupart. "A lithospheric instability origin for the Cameroon Volcanic Line." Earth and Planetary Science Letters 335-336 (June 2012): 80–87. http://dx.doi.org/10.1016/j.epsl.2012.04.028.

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17

Azinwi Tamfuh, Primus, Djibril Gus Kouankap Nono, Pierre Wotchoko, et al. "Geochemistry of a lateritic mantle developed on basalt in the Cameroon Western Highlands (Cameroon Volcanic Line)." Geoderma 376 (October 2020): 114569. http://dx.doi.org/10.1016/j.geoderma.2020.114569.

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18

Gountié Dedzo, Merlin, Djamilatou Diddi Hamadjoda, Eric Martial Fozing, et al. "Petrology and geochemistry of ignimbrites and associated enclaves from Mount Bambouto, West-Cameroon, Cameroon Volcanic Line." Geochemistry 80, no. 4 (2020): 125663. http://dx.doi.org/10.1016/j.chemer.2020.125663.

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19

Kamgang, Pierre, Emmanuel Njonfang, Alexandre Nono, Merlin Gountie Dedzo, and Félix M. Tchoua. "Petrogenesis of a silicic magma system: Geochemical evidence from Bamenda Mountains, NW Cameroon, Cameroon Volcanic Line." Journal of African Earth Sciences 58, no. 2 (2010): 285–304. http://dx.doi.org/10.1016/j.jafrearsci.2010.03.008.

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20

Gvoždík, Václav, Tadeáš Nečas, Matej Dolinay, Breda M. Zimkus, Andreas Schmitz, and Eric B. Fokam. "Evolutionary history of the Cameroon radiation of puddle frogs (Phrynobatrachidae: Phrynobatrachus), with descriptions of two critically endangered new species from the northern Cameroon Volcanic Line." PeerJ 8 (March 3, 2020): e8393. http://dx.doi.org/10.7717/peerj.8393.

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The Cameroon Volcanic Line, a mountain chain located between West and Central Africa, is a region of numerous endemic diversifications, including of puddle frogs (Phrynobatrachus). This study reviews the phylogeny and taxonomy of puddle frogs of the “Cameroon radiation,” which is a clade containing mainly montane but also at least three lowland species. Molecular data revealed a novel evolutionary lineage from high altitudes in the northern part of the mountains. Puddle frogs from the new, minute-sized (SVL < 20 mm) lineage are identified using molecular, morphological and acoustic data and

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21

Fokam, Joseph, Collins Ambe Chenwi, Desire Takou, et al. "Laboratory Based Surveillance of HIV-1 Acquired Drug Resistance in Cameroon: Implications for Use of Tenofovir-Lamivudine-Dolutegravir (TLD) as Second- or Third-Line Regimens." Viruses 15, no. 8 (2023): 1683. http://dx.doi.org/10.3390/v15081683.

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Increased HIV drug resistance (HIVDR) with antiretroviral therapy (ART) rollout may jeopardize therapeutic options, especially in this era of transition to fixed-dose tenofovir-lamivudine-dolutegravir (TLD). We studied acquired HIVDR (ADR) patterns and describe potentially active drugs after first- and second-line failure in resource-limited settings (RLS) like Cameroon. A laboratory-based study with 759 patients (≥15 years) experiencing virological failure was carried out at the Chantal Biya International Reference Centre (CIRCB), Yaoundé, Cameroon. Socio-demographic, therapeutic and immunovi

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22

Ekobo, Atanga. "Elephants in the Lobéké Forest, Cameroon." Pachyderm 19 (June 30, 1995): 73–80. http://dx.doi.org/10.69649/pachyderm.v19i1.812.

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Reviews results of dung counts by line transect ground surveys to ascertain the density of elephant in the Lobeke forest area. The data along with ecological surveys and other information is being utilized to assess the value of the forest area as a reserve.

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23

Onwubiko, Nwakuche Chinenye, Queen Ifeoma Emereola, Chinyere Prisca Anyanwu, and Grace Ovute Chimdi. "Preliminary study on species variability and evolutionary status of African walnut (Plukenetia conophora)." Acta Universitatis Sapientiae, Agriculture and Environment 13, no. 1 (2021): 77–87. http://dx.doi.org/10.2478/ausae-2021-0007.

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Abstract An analysis of the biochemical composition of African walnut seeds collected from two different geographical areas, Nigeria and Cameroon, was used to conduct the primary assessment of varietal differences and evolutionary status of Plukenetia conophora. The experiment was conducted at the Laboratory of Department of Biochemistry and Technology, Federal University of Technology, Owerri, Nigeria. The experimental design was completely randomized design with five replications. Significant difference (P > 0.05) was not observed with the proximate properties of the seeds of the two line

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24

Reusch, Angela Marie, Andrew A. Nyblade, Rigobert Tibi, et al. "Mantle transition zone thickness beneath Cameroon: evidence for an upper mantle origin for the Cameroon Volcanic Line." Geophysical Journal International 187, no. 3 (2011): 1146–50. http://dx.doi.org/10.1111/j.1365-246x.2011.05239.x.

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25

Reusch, A. M., A. A. Nyblade, D. A. Wiens, et al. "Upper mantle structure beneath Cameroon from body wave tomography and the origin of the Cameroon Volcanic Line." Geochemistry, Geophysics, Geosystems 11, no. 10 (2010): n/a. http://dx.doi.org/10.1029/2010gc003200.

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26

Njonfang, Emmanuel, and Alexandre Nono. "Clinopyroxene from some felsic alkaline rocks of the Cameroon Line, central Africa: petrological implications." European Journal of Mineralogy 15, no. 3 (2003): 527–42. http://dx.doi.org/10.1127/0935-1221/2003/0015-0527.

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27

Hlaváč, Peter, and Petr Baňař. "Pselaphinae of the Cameroon Volcanic Line. Part 1. New Pselaphinae (Coleoptera, Staphylinidae) from the island São Tomé." Zootaxa 5222, no. 3 (2022): 267–76. https://doi.org/10.11646/zootaxa.5222.3.4.

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Hlaváč, Peter, Baňař, Petr (2022): Pselaphinae of the Cameroon Volcanic Line. Part 1. New Pselaphinae (Coleoptera, Staphylinidae) from the island São Tomé. Zootaxa 5222 (3): 267-276, DOI: 10.11646/zootaxa.5222.3.4

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28

MANU, SHIIWUA, INAOYOM SUNDAY IMONG, and WILL CRESSWELL. "Bird species richness and diversity at montane Important Bird Area (IBA) sites in south-eastern Nigeria." Bird Conservation International 20, no. 3 (2010): 231–39. http://dx.doi.org/10.1017/s0959270909990311.

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SummaryThe mountains of south-eastern Nigeria are a western extension of the Cameroon mountain range, which is classified as an endemic bird area (EBA). Unlike its eastern extension in Cameroon, most of the ornithological surveys in the western extension of the Cameroon highlands in Nigeria have produced only limited checklists and inventories. There is a clear need for quantitative baseline data so that conservation problems can be identified. Twenty line transects covering a total transect length of 28.8 km were used to survey five sites (Afi Mountain Wildlife Sanctuary, Oban Division and Ok

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29

Moreau, C., J. M. Regnoult, B. Déruelle, and B. Robineau. "A new tectonic model for the Cameroon Line, Central Africa." Tectonophysics 141, no. 4 (1987): 317–34. http://dx.doi.org/10.1016/0040-1951(87)90206-x.

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30

Beh, Emmerencia Sih, and Nges Zillah Kimbeng. "Femininity vs Masculinity: Re-Defining (Gender) Roles in Alobwed’ Epie’s The Lady with a Beard." European Journal of Theoretical and Applied Sciences 2, no. 1 (2024): 96–106. http://dx.doi.org/10.59324/ejtas.2024.2(1).06.

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Gender bias has remained a pervasive problem worldwide, till this era. In line with the recent “UNDP Gender Inequality Index” which ranks Cameroon 141st among a total of 162 classified world countries, Cameroon is determined a heavily patriarchal society. Developing gender as a social construction rather than a biological attribute is a powerful achievement that determines roles being awarded accordingly and not based on genetic traits. The foregoing declarations put this paper in perspective. Gender can grow beyond any limit if it is not tied down to sex. Therefore, gender should be redefined

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Emmerencia, Sih Beh. "Femininity vs Masculinity: Re-Defining (Gender) Roles in Alobwed' Epie's The Lady with a Beard." European Journal of Theoretical and Applied Sciences 2, no. 1 (2024): 96–106. https://doi.org/10.59324/ejtas.2024.2(1).06.

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Gender bias has remained a pervasive problem worldwide, till this era. In line with the recent “UNDP Gender Inequality Index” which ranks Cameroon 141st among a total of 162 classified world countries, Cameroon is determined a heavily patriarchal society. Developing gender as a social construction rather than a biological attribute is a powerful achievement that determines roles being awarded accordingly and not based on genetic traits. The foregoing declarations put this paper in perspective. Gender can grow beyond any limit if it is not tied down to sex. Therefore, gender should

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32

Couvreur, Thomas L. P., Leo-Paul M. J. Dagallier, Francoise Crozier, et al. "Flora of Cameroon – Annonaceae Vol 45." PhytoKeys 207 (September 20, 2022): 1–532. http://dx.doi.org/10.3897/phytokeys.207.61432.

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Annonaceae is a major pantropical family with 113 genera and about 2550 species. Cameroon is one of the most biodiverse countries in Africa but its flora remains incompletely known. In this volume of the Flora of Cameroon, we describe 166 native taxa representing 163 species in 28 native genera within the family Annonaceae. A total of 22 species (about 13%) are endemic to the country. We provide keys to all native genera, species, and infraspecific taxa. For each species a detailed morphological description and a map of its distribution in Cameroon are provided. Distribution maps and diversity

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33

ZANGMO, Ghislain T., Armand D. KAGOU, David G. NKOUATHIO, and Pierre WANDJI. "Typology of Natural Hazards and Assessment of Associated Risks in the Mount Bambouto Caldera (Cameroon Line, West Cameroon)." Acta Geologica Sinica - English Edition 83, no. 5 (2009): 1008–16. http://dx.doi.org/10.1111/j.1755-6724.2009.00130.x.

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34

Ngwa, Caroline N., Bless N. Shu, Benoît J. Mbassa, Festus T. Aka, and Pauline N. Wokwenmendam. "Olivine chemistry from Cameroon: evidence of carbonate metasomatism along the ocean-continental boundary of the Cameroon volcanic line." Mineralogy and Petrology 114, no. 1 (2019): 57–70. http://dx.doi.org/10.1007/s00710-019-00689-5.

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35

Ako, Andrew Ako, Gloria Eneke Takem Eyong, Jun Shimada, et al. "Nitrate contamination of groundwater in two areas of the Cameroon Volcanic Line (Banana Plain and Mount Cameroon area)." Applied Water Science 4, no. 2 (2013): 99–113. http://dx.doi.org/10.1007/s13201-013-0134-x.

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36

van der Geest, Sjaak. "‘Criminaliteit’ als normaliteit." Tijdschrift over Cultuur & Criminaliteit 14, no. 3 (2024): 25–40. https://doi.org/10.5553/tcc/221195072024014003003.

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Criminality as normality – About distribution of medicines in Cameroon 1980 This article is based on participant-observational field research in Cameroon in 1980. It originally focused on what happened to sick people and their relatives at the end of the medicine distribution line. However, the investigation led directly to higher levels of the medicine trade: the informal drug seller in markets and general stores, the licensed legal pharmacies, the hospitals and health centres, the National Pharmacy, and finally the shadowy world of policy makers negotiating with the pharmaceutical companies.

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37

Njom‐Nlend, Anne‐Esther, Nadège Efouba, Arsène Brunelle Sandie, and Joseph Fokam. "Determinants of switch to paediatric second‐line antiretroviral therapy after first‐line failure in Cameroon." Tropical Medicine & International Health 26, no. 8 (2021): 927–35. http://dx.doi.org/10.1111/tmi.13595.

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38

Aminatou, Fagny Mefire, Nkouandou Oumarou Faarouk, Temdjim Robert, et al. "New K–AR ages of tchabal mbabo alkaline volcano massif, Cameroon volcanic line and adamawa plateau (central Africa)." International Journal of Advanced Geosciences 4, no. 2 (2016): 62. http://dx.doi.org/10.14419/ijag.v4i2.6516.

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Tchabal Mbabo in Central Africa is a voluminous volcano massif composed of alkali lava series. K-Ar geochronology data obtained from three samples of basanite - trachyandesite composition defined at least two volcanic activities. The first at end Eocene (38.22 ± 0.80 Ma) and the second during Oligocene (28.88 ± 0.61 and 28.60 ± 0.60Ma). The distribution of different ages along the Cameroon Volcanic Line is difficult to council with any migration of magmatic activity, as previously suggested. The most realistic scenario for the formation of Cameroon Line is that the ascent of lavas has been fav

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39

Dedzo, Merlin Gountié, Pierre Kamgang, Emmanuel Njonfang, and Ghislain Zangmo Tefogoum. "Hazards from Pyroclastic Density Currents at Mount Bamenda (West-Cameroon, Cameroon Volcanic Line): Mapping and Assessment by AMS Method." American Journal of Geoscience 5, no. 2 (2015): 26–39. http://dx.doi.org/10.3844/ajgsp.2015.26.39.

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40

Njonfang, Emmanuel, and Christian Moreau. "The mineralogy and geochemistry of a subvolcanic alkaline complex from the Cameroon Line: The Nda Ali massif, southwest Cameroon." Journal of African Earth Sciences 22, no. 2 (1996): 113–32. http://dx.doi.org/10.1016/0899-5362(96)00126-1.

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41

Donald Ngonge, E., Maria Helena B. M. Hollanda, E. Nkonguin Nsifa, and Felix M. Tchoua. "Petrology of the Guenfalabo ring-complex: An example of a complete series along the Cameroon Volcanic Line (CVL), Cameroon." Journal of African Earth Sciences 96 (August 2014): 139–54. http://dx.doi.org/10.1016/j.jafrearsci.2014.03.027.

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42

Chongwain, Gilbert Mbzighaa, Christopher M. Agyingi, J. Foba-Tendo, and A. F. Epanty. "Sedimentology and geochemistry of carbonate bearing-argillites on the southeastern flank of mount Cameroon (likomba), Cameroon volcanic line (CVL)." Journal of African Earth Sciences 156 (August 2019): 178–88. http://dx.doi.org/10.1016/j.jafrearsci.2019.04.010.

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43

HLAVÁČ, PETER, PETR BAŇAŘ, and ERIC BERTRAND FOKAM. "Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon." Zootaxa 5323, no. 2 (2023): 255–67. http://dx.doi.org/10.11646/zootaxa.5323.2.5.

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The new genus and species, Ewoma longiscapa gen. et sp. nov. of the pselaphine tribe Goniacerini based on specimens collected on Mount Cameroon are described and illustrated. The taxonomic position of the new genus within the tribe Goniacerini is discussed. The list of all genera of Goniacerini of sub-Saharan continental Africa with the number of species and the distribution as well as the list of all species known from Western Africa are given. The short overview of our knowledge of studies of the Pselaphinae of the sub-Saharan continental Africa is also provided.

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44

Yamgouot, Fadimatou Ngounouno, Bernard Déruelle, Isaac Bertrand Gambie Mbowou, and Ismaïla Ngounouno. "Petrology of the Volcanic Rocks from Bioko Island (“Cameroon Hot Line”)." International Journal of Geosciences 06, no. 03 (2015): 247–55. http://dx.doi.org/10.4236/ijg.2015.63019.

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45

Ballentine, C. J., D. C. Lee, and A. N. Halliday. "Hafnium isotopic studies of the Cameroon line and new HIMU paradoxes." Chemical Geology 139, no. 1-4 (1997): 111–24. http://dx.doi.org/10.1016/s0009-2541(97)00028-4.

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46

Itiga, Zénon, Jacques-Marie Bardintzeff, Pierre Wotchoko, Pierre Wandji, and Hervé Bellon. "Tchabal Gangdaba massif in the Cameroon Volcanic Line: a bimodal association." Arabian Journal of Geosciences 7, no. 11 (2013): 4641–64. http://dx.doi.org/10.1007/s12517-013-1126-8.

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47

Aka, Festus T., Keisuke Nagao, Minoru Kusakabe, et al. "Symmetrical Helium isotope distribution on the Cameroon Volcanic Line, West Africa." Chemical Geology 203, no. 3-4 (2004): 205–23. http://dx.doi.org/10.1016/j.chemgeo.2003.10.003.

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Djoda, Bello, Patrick Valere Tsouh Fokou, Patrick Achiangia Njukeng, et al. "Antiretroviral drug resistance in HIV-1 patients on first-line therapy or untreated across five treatment centers in Yaounde's Centre Region, Cameroon." Journal of Drug Delivery and Therapeutics 15, no. 5 (2025): 86–99. https://doi.org/10.22270/jddt.v15i5.7126.

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Abstract:

Antiretroviral therapy (ART) improves HIV survival. However, as ART programs expand in resource-limited settings like Cameroon toward UNAIDS 95-95-95 goals, monitoring drug resistance is critical. This study investigated HIV-1 subtypes and resistance mutations in Yaoundé, Cameroon. From 2017 to 2021, 231 HIV-positive individuals (treatment-naïve and ART-experienced patients with virological failure [viral load >1,000 copies/mL]) were enrolled across five clinics. Plasma samples were sequenced for reverse transcriptase (RT) and protease (PR) genes. Participants were predominantly female (67.

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Kamgang, Pierre, Gilles Chazot, Emmanuel Njonfang, Nicaise Blaise Tchuimegnie Ngongang, and Félix M. Tchoua. "Mantle sources and magma evolution beneath the Cameroon Volcanic Line: Geochemistry of mafic rocks from the Bamenda Mountains (NW Cameroon)." Gondwana Research 24, no. 2 (2013): 727–41. http://dx.doi.org/10.1016/j.gr.2012.11.009.

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Fagny, A. M., O. F. Nkouandou, J. M. Bardintzeff, et al. "Petrology and geochemistry of the Tchabal Mbabo volcano in Cameroon volcanic line (Cameroon, Central Africa): An intra-continental alkaline volcanism." Journal of African Earth Sciences 170 (October 2020): 103832. http://dx.doi.org/10.1016/j.jafrearsci.2020.103832.

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