Éditeur(s) : Academic Affairs Library, University of North Carolina at Chapel Hill Academic Affairs Library, University of North Carolina at Chapel Hill ( [Chapel Hill, N.C.] )
Résumé : (Statement of Responsibility) interspers'd throughout with several historical remarks on the commerce of the European Nations, whose subjects frequent the Coast of Guinea. To which is prefixed a letter from the Author to a Person of Distinction, in reference to some natural curiosities in Africa, as well as explaining the motives which induced him to compose these memoirs.
(Original Version) Transcribed from: London : Printed for W. Reeve, [1750?] 55 p. The Royal African, or, Memoirs of the Young Prince of Annamaboe : comprehending a distinct account of his country and family : his elder brother's voyage to France, and reception there : the manner in which himself was confided by his father to the Captain who sold him : his condition while a slave in Barbadoes : the true cause of his being redeemed : his voyage from thence : and reception here in England / interspers'd throughout with several historical remarks on the commerce of the European Nations, whose subjects frequent the Coast of Guinea. To which is prefixed a letter from the Author to a Person of Distinction, in reference to some natural curiosities in Africa, as well as explaining the motives which induced him to compose these memoirs. 2nd ed.
(Funding) Funding from the University Library, University of North Carolina at Chapel Hill supported the electronic publication of this title.
(System Details) Mode of access: Internet World Wide Web.
Title from electronic title page (viewed June 14, 2004).
This electronic edition is part of the UNC-CH digitization project's database, Documenting the American South. It is a part of the collection North American slave narratives.
Text transcribed by Apex Data Services, Inc. Images scanned by Elizabeth S. Wright. Text encoded by Apex Data Services, Inc. and Elizabeth S. Wright.
Item in DocSouth.
Early Caribbean Digital Archive.
Africa
Africa, West
Great Britain
Africa, West

57188847
ocm57188847
http://ufdc.ufl.edu/AA00015399/00001

Éditeur(s) : Academic Affairs Library, University of North Carolina at Chapel Hill Academic Affairs Library, University of North Carolina at Chapel Hill ( [Chapel Hill, N.C.] )
Résumé : (Statement of Responsibility) written and revised from his own words by Samuel Moore.
(Original Version) Transcribed from the photocopy of: Detroit : Printed for the author, Mahommah Gardo Baquaqua, by Geo. E. Pomeroy & Co., Tribune office, 1854. 66 p. ; 22 cm. Biography of Mahommah G. Baquaqua : a native of Zoogoo, in the interior of Africa (a convert of Christianity), with a description of that part of the world, including the manners and customs of the inhabitants ... Mahommah's early life, his education, his capture and slavery in Western Africa and Brazil, his escape to the United States, from thence to Hayti, (the city of Port Au Prince,) his reception by the Baptist Missionary there, the Rev. W.L. Judd; his conversion to Christianity, Baptism, and return to this country, his views, objects and aim / written and revised from his own words by Samuel Moore, ESQ., late publisher of the "North of England Shipping Gazette," author of several popular works, and editor of sundry reform papers. Cover title: An interesting narrative : biography of Mahommah G. Baquaqua ...|"Prayer of the oppressed"--P. [66].
(Funding) Funding from the National Endowment for the Humanities supported the electronic publication of this title.
(System Details) Mode of access: Internet World Wide Web.
(System Details) System requirements: PC with modem or direct Internet connection; SGML viewer required for SGML files.
Title from electronic title page.
This electronic edition has been transcribed from a photocopy supplied by the North Carolina State University Library.
Includes information about Central Africa "their religious notions, form of government, laws, appearance of the country, buildings, agriculture, manufactures, shepherds and herdsmen, domestic animals, marriage ceremonials, funeral services, styles of dress, trade and commerce, modes of warfare, system of slavery, &c., &c."
This electronic edition is part of the UNC-CH digitization project's database, Documenting the American South. It is a part of the collection North American slave narratives.
Text transcribed by Apex Data Services, Inc. Text encoded by Apex Data Services, Inc., Elizabeth S. Wright and Natalia Smith.
Early Caribbean Digital Archive.
Africa
Africa
Brazil
Africa, Central
Africa, Central

Droits : See: http://docsouth.unc.edu/neh/baquaqua/menu.html
48112283
ocm48112283
http://ufdc.ufl.edu/AA00015610/00001

Éditeur(s) : Printed by John Baskett, Printer to the King's most Excellent Majesty Printed by John Baskett, Printer to the King's most Excellent Majesty
Résumé : The West Indies were colonized by Great Britain beginning in the early 17th century and were crucial to the triangular trade that developed between Europe, Africa, and the British colonies of North America and the Caribbean. The acts in the collection often address issues of trade, both between the islands and between the islands and Great Britain during the 18th and 19th centuries
The entire collection is open for research.
Cite as: Bryant British West Indies British Parliamentary Acts Collection, Special Collections and University Archives, University of Central Florida Libraries, Orlando, Florida.
Unpublished records are protected by copyright. Permission to publish quote or reproduce must be secured from the repository and the copyright holder.

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM2002_08
DP0001149

Éditeur(s) : Université des Antilles AIHP-GEODE : Archéologie Industrielle, Histoire, Patrimoine/Géographie- Développement Environnement de la Caraïbe HARCMAR : Histoire et Archéologie Maritimes des Petites Antilles
Extrait de : "Entre exclusif et contrebande, le commerce colonial aux Antilles XVIIe-début XIXe siècle" : journées d'étude, du 24 au 26 octobre 2019. Université des Antilles
Description : In the eighteenth and the early nineteenth centuries, inter-imperial connections, many of which were illicit, were of crucial importance in the functioning of European colonialism in the Atlantic world and during its heyday. One example of economically important trade connections across imperial borders is the maritime mule trade. Based on a large variety of secondary sources, supplemented by primary materials, this paper seeks to provide insights into the functioning of this business. Enterprising merchants used the opportunities available to them to connect breeding areas and zones of cash crop production. Likewise, geography played an important role in connecting demand and supply over both short and long distances, as physical proximity and trade winds helped forge connections. Mules were transported to the insular Caribbean, and in particular the French islands, to serve as draft animals, especially by moving vertical cylinders called rollers that crushed the sugar cane, although they were not the only animals used for such purposes. To meet the mule demand of the Caribbean islands, the animals were imported from a variety of regions, including France, North Africa, and the Cape Verde islands. Eventually, however, supplies from other parts of the Greater Caribbean came to dominate the mule business.
Siècle(s) traité(s) : 18
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V19112
V19112

Éditeur(s) : Printed by C. Eyre and the Executors of W. Strahan, Printers to the King's most Excellent Majesty Printed by C. Eyre and the Executors of W. Strahan, Printers to the King's most Excellent Majesty
Résumé : The West Indies were colonized by Great Britain beginning in the early 17th century and were crucial to the triangular trade that developed between Europe, Africa, and the British colonies of North America and the Caribbean. The acts in the collection often address issues of trade, both between the islands and between the islands and Great Britain during the 18th and 19th centuries.
The entire collection is open for research.
Cite as: Bryant British West Indies British Parliamentary Acts Collection, Special Collections and University Archives, University of Central Florida Libraries, Orlando, Florida
Unpublished records are protected by copyright. Permission to publish quote or reproduce must be secured from the repository and the copyright holder

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM2002_08
DP0001172

Éditeur(s) : American Geophysical Union
Résumé : As part of the French CLIPPER project, an eddy permitting model of the Atlantic circulation has been run for 22 years. The domain has open boundaries at Drake passage and at 30 degreesE, from Africa to Antarctica. The simulated mean circulation, as well as the eddy activity, is satisfactory for a 1/3 degrees model resolution, and the meridional heat transport at 30 degreesS is within the range estimated from observations. We use the "mixed" open boundary algorithm of Barnier et al. [1998], which has both a radiation condition and a relaxation to climatology. The climatological boundary forcing strongly constrains the solution in the whole domain. The model heat balance adjusts through the surface (heat flux retroaction term) more than the open boundaries. The radiation phase velocities calculated within the algorithm are analyzed. This shows, quite surprisingly, that both the eastern and western boundaries have a similar behavior, regardless of the preferred directions for advection (mainly eastward) and wave propagation (mainly westward). Our results confirm that open boundary algorithms behave differently according to the dynamics of the region considered. The passive boundary condition that Penduff et al. [2000] applied successfully in the north eastern Atlantic does not work in the present South Atlantic model. We emphasize the need for a careful prescription of the climatology at the open boundary, for which a new approach based on synoptic sections is implemented.
Journal of Geophysical Union - Research C - Oceans (0148-0227) (American Geophysical Union), 2001-10 , Vol. 106 , N. C10 , P. 22115-22129

Droits : 2001 American Geophysical Union
http://archimer.ifremer.fr/doc/2001/publication-454.pdf
DOI:10.1029/2000JC000376
http://archimer.ifremer.fr/doc/00000/454/

Éditeur(s) : Printed by Charles Eyre and William Strahan, Printers to the King's most Excellent Majesty Printed by Charles Eyre and William Strahan, Printers to the King's most Excellent Majesty
Résumé : The West Indies were colonized by Great Britain beginning in the early 17th century and were crucial to the triangular trade that developed between Europe, Africa, and the British colonies of North America and the Caribbean. The acts in the collection often address issues of trade, both between the islands and between the islands and Great Britain during the 18th and 19th centuries.
The entire collection is open for research.
Cite as: Bryant British West Indies British Parliamentary Acts Collection, Special Collections and University Archives, University of Central Florida Libraries, Orlando, Florida.
Unpublished records are protected by copyright. Permission to publish quote or reproduce must be secured from the repository and the copyright holder.

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM2002_08
DP0001162

Éditeur(s) : Printed by Charles Eyre and William Strahan, Printers to the King's most Excellent Majesty Printed by Charles Eyre and William Strahan, Printers to the King's most Excellent Majesty
Résumé : The West Indies were colonized by Great Britain beginning in the early 17th century and were crucial to the triangular trade that developed between Europe, Africa, and the British colonies of North America and the Caribbean. The acts in the collection often address issues of trade, both between the islands and between the islands and Great Britain during the 18th and 19th centuries.
The entire collection is open for research.
Cite as: Bryant British West Indies British Parliamentary Acts Collection, Special Collections and University Archives, University of Central Florida Libraries, Orlando, Florida.
Unpublished records are protected by copyright. Permission to publish quote or reproduce must be secured from the repository and the copyright holder.

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM2002_08
DP0001166

Éditeur(s) : HAL CCSD BMJ Publishing Group
Résumé : International audience
BACKGROUND: Mutations in the leucine-rich-repeat kinase 2 (LRRK2) gene have been identified in families with autosomal dominant Parkinson's disease (ADPD), the most common of which is the p.G2019S substitution that has been found at varying frequencies worldwide. Because of the size of the LRRK2 gene, few studies have analysed the entire gene in large series of ADPD families. METHODS: We performed extensive mutation analyses of all 51 coding exons of the LRRK2 gene in index cases from 226 Parkinson's disease families compatible with autosomal dominant inheritance, mostly from France (n = 182) and North Africa (n = 14). RESULTS: We found 79 sequence variants, 29 of which were novel. Eight potentially or proven pathogenic mutations were found in 22 probands (9.7%). There were four novel amino acid substitutions that are potentially pathogenic (p.S52F, p.N363S, p.I810V, p.R1325Q) and two novel variants, p.H1216R and p.T1410M, that are probably not causative. The common p.G2019S mutation was identified in 13 probands (5.8%) including six from North Africa (43%). The known heterozygous p.R1441H and p.I1371V mutations were found in two probands each, and the p.E334K variant was identified in one single patient. Most potentially or proven pathogenic mutations were located in the functional domains of the Lrrk2 protein. CONCLUSION: This study leads us to conclude that LRRK2 mutations are a common cause of autosomal dominant Parkinson's disease in Europe and North Africa.
ISSN: 0022-2593

inserm-00529272
http://www.hal.inserm.fr/inserm-00529272
DOI : 10.1136/jmg.2008.062612
PUBMED : 19357115

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
Although advanced anthropoid primates (i.e., Simiiformes) are recorded at the end of the Eocene in North Africa (Proteopithecidae, Parapithecidae, and Oligopithecidae), the origin and emergence of this group has so far remained undocumented. The question as to whether these primates are the result of a monophyletic radiation of endemic anthropoids in Africa, or several Asian clades colonizing Africa, is a current focus of paleoprimatology. In this article, we report the discovery of a new anthropoid from Djebel el Kébar in central Tunisia, dating from the late middle Eocene (Bartonian). This taxon, Amamria tunisiensis, new genus and species, currently known by only one isolated upper molar, is among the most ancient anthropoids to be recorded in Africa thus far. Amamria displays a suite of dental features that are primarily observed in Eosimiiformes (stem Anthropoidea). However, it is not allocated to any known family of that group (i.e., Asian Eosimiidae and Afro-Asian Afrotarsiidae) inasmuch as it develops some dental traits that are unknown among eosimiiforms, but can be found in African simiiform anthropoids such as proteopithecids and oligopithecids. With such a mosaic of dental traits, Amamria appears to be a structural intermediate, and as such it could occupy a key position, close to the root of the African simiiforms. Given its antiquity and its apparent pivotal position, the possibility exists that Amamria could have evolved in Africa from Asian eosimiiform or Asian "proto"-simiiform ancestors, which would have entered Africa sometime during the middle Eocene. Amamria could then represent one of the earliest offshoots of the African simiiform radiation. This view would then be rather in favor of the hypothesis of a monophyletic radiation of endemic simiiform anthropoids in Africa. Finally, these new data suggest that there must have been at least two Asian anthropoid colonizers of Africa: the afrotarsiids and the ancestor of Amamria.
ISSN: 0002-9483

hal-01053704
https://hal.archives-ouvertes.fr/hal-01053704
DOI : 10.1002/ajpa.22523

Éditeur(s) : Copernicus Gesellschaft Mbh
Résumé : Deep-sea bivalves found at hydrothermal vents, cold seeps and organic falls are sustained by chemosynthetic bacteria which ensure part or all of their carbon nutrition. These symbioses are of prime importance for the functioning of the ecosystems. Similar symbioses occur in other bivalve species living in shallow and coastal reduced habitats worldwide. In recent years, several deep-sea species have been investigated from continental margins around Europe, West Africa, East America, the Gulf of Mexico, and from hydrothermal vents on the Mid-Atlantic Ridge. In parallel, numerous more easily accessible shallow marine species were studied. We here provide a summary of the current knowledge available on chemosymbiotic bivalves in the area ranging west-to-east from the Gulf of Mexico to Marmara Sea, and north-to-south from the Arctic to the Gulf of Guinea. Characteristics of symbioses in 51 species from the area are summarized for each of the five bivalve families documented to harbor chemosynthetic symbionts (Mytilidae, Vesicomyidae, Solemyidae, Thyasiridae and Lucinidae), and compared among families with special emphasis on ecology, life cycle, and connectivity. Chemosynthetic symbioses are a major adaptation to ecosystems and habitats exposed to reducing conditions, yet relatively little is known regarding their diversity and functioning apart from a few "model species" on which effort has focused over the last 30 yr. In the context of increasing concern about biodiversity and ecosystems, and increasing anthropogenic pressure on Oceans, we advocate for a better assessment of bivalve symbioses diversity in order to evaluate the capacities of these remarkable ecological and evolutionary units to withstand environmental change
Biogeosciences (1726-4170) (Copernicus Gesellschaft Mbh), 2013 , Vol. 10 , N. 5 , P. 3241-3267

Droits : Author(s) 2012. CC Attribution 3.0 License.
http://archimer.ifremer.fr/doc/00133/24417/22431.pdf
DOI:10.5194/bg-10-3241-2013
http://archimer.ifremer.fr/doc/00133/24417/

Résumé : The study conducted in the framework of an agreement between Ifremer and the Local fisheries committee at Audierne is part of a project to restore spiny lobster Palinurus elephas stock levels in the Iroise Sea. It is supported by professional fishermen from Finistère and by the Regional fisheries committee of Brittany. After a brief review of the way lobster stocks are managed worldwide, followed by the major biological and ecological features of red lobster and the state of fisheries in Europe and North Africa, the very poor state of the resource along French coast is borne out by the statistics of landings. Various scenarios (not alternatives) to promote the rebuilding of the biomass are suggested: minimum landing size increase, seasonal closure of the fishery, berried females protection, no fishing zones. The drift of phyllosoma larvae during their long larval stage is addressed using a 3-D hydrodynamic simulation model.
L'étude réalisée dans le cadre d'une convention entre Ifremer et le Comité local des Pêches d'Audierne s'inscrit dans un projet de reconquête des niveaux de ressource en langouste rouge Palinurus elephas en mer d'Iroise soutenu par les pêcheurs professionnels de la pointe du Finistère et par le Comité régional des Pêches de Bretagne. Après avoir rappelé brièvement les modalités de gestion des stocks de langoustes dans le monde puis les grands traits biologiques et écologiques de la langouste rouge et l'état des pêcheries en Europe et dans le nord de l'Afrique, le très mauvais état de cette ressource sur les côtes françaises est confirmé au travers des statistiques de débarquement. Divers scénarios (non alternatifs) visant à favoriser la reconstitution d'une biomasse sont proposés : augmentation de la taille minimale au débarquement, fermeture saisonnière de la pêche, protection des femelles ovigères et création de zones protégées. La dérive des larves phyllosomes au cours de leur longue phase larvaire est abordée par un modèle de simulation hydrodynamique en trois dimensions.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/2005/rapport-1198.pdf
http://archimer.ifremer.fr/doc/00000/1198/

Éditeur(s) : HAL CCSD
Résumé : International audience
Coming from Crimea, the Black Death spread to Western Europe and North Africa during the 1340s. From 1346 to 1352, the plague killed an estimated 25-40% of Europeans of all age-groups [1] , i.e., 30 to 60% of Europe population. One of the earliest and most widely accepted explanations was that God was punishing humanity for their sins. One remedy for the curse was to do penitence. Thus in 1348 there rapidly arose a mass movement of flagellation [2]. In fact flagellation could not really help against such threat. The Black Death or Bubonic plague is caused by Yersinia pestis, a Eubacteria discovered in 1894 by Alexandre Yersin. It is transmitted by the bite of the flea Xenopsylla cheopsis. This flea lives by feeding the blood of many species besides man but its most preferred relationship is with the black rat (Rattus rattus). Fossilized remains of the plague flea have been found in large numbers in Amarna, Egypt [3, 4] about 1350 BC, and thus could be directly linked to the events described in the Book of Samuel [5, 6]. During the epidemic of Bubonic plague in London in 1665-1666, the known treatments were made use of, e.g. the so-famous Theriac or Venice Treacle which is used from the time of ancient Rome as a remedy against poison [7]. Since then, more specialized and novel treatments have been developed. However, since the characterization of Yersinia pestis, numerous drugs have been developed against it, e.g. gentamicin or doxycycline [8]. These researches had been carried out using more elaborated biochemical, biophysical and biological approaches.
Infectious disorders drug targets

Droits : info:eu-repo/semantics/OpenAccess
inserm-00395256
http://www.hal.inserm.fr/inserm-00395256
http://www.hal.inserm.fr/inserm-00395256/document
http://www.hal.inserm.fr/inserm-00395256/file/editorial.pdf
http://www.hal.inserm.fr/inserm-00395256/file/inserm-00395256_edited.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Holocene Lake Mega-Chad (LMC) was the largest late Quaternary water-body in Africa. The development of this giant paleo-lake is related to a northward shift of the isohyetes interpreted as evidence for an enhanced Monsoon (African Humid Period). Numerous preserved coastal features have been described all around the LMC shore. Such features reveal the main paleo-hydrodynamical tendencies. In the context of a closed water-body like LMC, hydrodynamics are forced mainly by winds. We use a three-dimensional numerical model (SYMPHONIE) to simulate the mean hydrodynamics in LMC under both Harmattan-like (northeasterly trade winds) and Monsoon-like (southwesterly winds) forcings. The northern part of LMC displays coastal features, such as sand spits, that are consistent with the simulations forced by Harmattan-like winds. Geomorphic features related to Monsoon-driven hydrodynamics are not clearly expressed. They could have developed during the early stage of LMC but subsequently reworked. At the time of sand-spit building, Harmattan-like driven hydrodynamics prevailed and related coastal features were preferentially preserved in the sedimentary record.
ISSN: 0033-5894

hal-00475633
https://hal.archives-ouvertes.fr/hal-00475633
DOI : 10.1016/j.yqres.2009.10.010

Éditeur(s) : HAL CCSD Elsevier
Résumé : This paper is the first presentation of a project called GHYRAF (Gravity and Hydrology in Africa) devoted to the detailed comparison between models and multidisciplinary observations (ground and satellite gravity, geodesy, hydrology, meteorology) of the variations of water storage in Africa from the Sahara and part to the monsoon equatorial part. We describe the various actions planned in this project. We first detail the actions planned in gravimetry which consist in two main surface gravity experiments: on the one hand the periodic repetition of absolute gravity measurements along a north-south monsoonal gradient of rainfall in West Africa, going from Tamanrasset (20 mm/year) in southern Algeria to Djougou (1200 mm/year) in central Benin; on the other hand the continuous measurements at Djougou (Benin) with a superconducting gravimeter to monitor with a higher sampling rate the gravity changes related to an extreme hydrological cycle. Another section describes the actions planned in GPS which will maintain and develop the present-day existing network in West Africa. The third type of actions deals with hydrology and we review the three sites that will be investigated in this joint hydrogeophysics project namely Wankama (near Niamey) and Bagara (near Diffa) in the Niger Sahelian zone and Nalohou (near Djougou) in the Benin monsoon zone. We also address the question of the ground truth of satellite-derived missions: in this context the GHYRAF project will lead to test the hydrology models by comparison both with in situ and satellite data such as GRACE, as well as to an important increase of our knowledge of the seasonal water cycle in Africa. We finally present preliminary results in GPS based on the analysis of the vertical motion of the Djougou site. The resulting absolute gravity changes related to the 2008 monsoon are finally given.
ISSN: 0264-3707

hal-00475660
https://hal.archives-ouvertes.fr/hal-00475660
DOI : 10.1016/j.jog.2009.09.014

Éditeur(s) : HAL CCSD Ocean Drilling Programm
Résumé : This paper provides a summary of postcruise scientific results from Ocean Drilling Program (ODP) Leg 209 available to date, building upon shipboard observations and syntheses summarized in the Leg 209 Initial Results volume. During Leg 209, 19 holes were drilled at 8 sites along the Mid-Atlantic Ridge from 14°43´ to 15°44´N, mainly in residual mantle peridotite intruded by gabbroic rocks, in order to understand the tectonic and structural processes responsible for formation of oceanic lithosphere with abundant residual peridotite exposed on the seafloor coupled with a relatively low proportion of volcanic rocks. Based on proportions of recovered lithologies, the entire area may be underlain by mantle peridotite with ~20%–40% gabbroic intrusions and impregnations. Impregnated peridotites with olivine + two pyroxenes + plagioclase + spinel that apparently formed in equilibrium probably record crystallization from primitive mid-ocean-ridge basalt at pressures of 0.5–0.6 GPa. Metamorphic equilibria record isobaric cooling to ~1100°C at this pressure. Thus, the conductively cooled thermal boundary layer beneath the Mid-Atlantic Ridge in this region is >15 km thick. Combined crystallization and reaction with residual peridotite formed a series of impregnated peridotites recording increasing Na content at nearly constant Mg#; this process could explain some of the variation in fractionation-corrected Na (e.g., Na = 8.0) observed in mid-ocean-ridge basalts. Clinopyroxene textures and compositions record such impregnation processes, and they are particularly well documented for Site 1274. Other Leg 209 gabbroic rocks formed from extensive crystallization of highly evolved melts, indicating that a substantial proportion of melt entering the thermal boundary layer crystallizes entirely beneath the seafloor, with no volcanic equivalent. Alteration of peridotites occurred over a range of temperatures and is the result of three distinct processes: rock-dominated serpentinization with formation of brucite in olivine-rich lithologies, fluid-dominated serpentinization with formation of magnetite and no brucite, and fluid-dominated talc alteration with addition of SiO2 as well as H2O and oxygen. The latter two processes also exhibit detectable trace element metasomatism that is distinct in its character from the igneous impregnation described in the previous paragraph. Microstructures show that most residual peridotites were not ductilely deformed at temperatures less than ~1200°C. Structural and paleomagnetic data require tectonic rotations of relatively undeformed blocks; some rotations probably exceeded 60° around nearly horizontal axes parallel to the rift axis. Rotations occurred along several generations of high-temperature mylonitic shear zones extending deeper than 15 km depth and numerous faults at lower temperature. Early formed shear zones and faults were passively rotated around later features; such a process could have produced low-angle fault surfaces without slip on low-angle faults. This region provides end-member examples of processes that are common at many or most slow-spreading ridges. Osmium isotope ratios indicate an ancient history of depletion for residual peridotites from the 14°–16°N region along the Mid-Atlantic Ridge. Though depleted Os isotope ratios in peridotite have been reported elsewhere along the global ridge system, the values from this region are among the most depleted. In general, Os isotope ratios from mid-ocean-ridge basalts are systematically more radiogenic than Os isotope ratios from ridge peridotite samples, suggesting a polygenetic heterogeneous source for mid-ocean-ridge basalts. Geochemical studies of zircons from Leg 209 gabbroic rocks and impregnated peridotites, together with other ridge and arc-related zircons, indicate that ridge zircons have systematically lower fractionation-corrected U and Th concentrations compared to arc zircons. This observation provides a tool for interpreting the tectonic provenance of ancient detrital zircons and indicates an arclike provenance for Hadean detrital zircons. Geobiological studies and aerobiological studies were also undertaken during Leg 209. The geobiological work found no measurable microbial enhancement of olivine dissolution rate, possibly because the samples from Leg 209 were sterile. The aerobiological study determined that dust from North Africa, collected from the derrick of the JOIDES Resolution during Leg 209, contains a variety of abundant microorganisms.
Proceedings ODP, scientific results, 209

hal-00407966
https://hal.archives-ouvertes.fr/hal-00407966
DOI : 10.2973/odp.proc.sr.209.001.2007

Éditeur(s) : HAL CCSD Geological Society of London
Résumé : The Borborema and Benin–Nigeria provinces of NE Brazil and NW Africa, respectively, are key areas in the amalgamation of West Gondwana by continental collision during the Brasiliano/Pan-African orogenies. Both are underlain by complex basement: Nigeria has c. 3.05 Ga Archaean crust but no known Palaeoproterozoic rocks >2.0 Ga; in NE Brazil, 2.6–3.5 Ga Archaean rocks form small cores within Palaeoproterozoic gneiss terrains affected by plutonism at c. 2.17 Ga. Both regions exhibit Late Palaeoproterozoic (c. 1.8 Ga) rift-related magmatism and metasedimentary sequences overlying the basement. The Seridó Group of NE Brazil (<0.65 Ga) is similar to the Igarra Sequence in SW Nigeria. The Ceará Group, which may date back to c. 0.85 Ga, is a passive margin deposit on crust thinned during initiation of an oceanic domain. In both provinces, basement and sedimentary cover were involved in tangential tectonics that resulted in crust-thickening by nappe-stacking associated with closure of this ocean. Frontal collision between c. 0.66 and 0.60 Ga later evolved to an oblique collision, generating north–south continental strike-slip shear zones at c. 0.59 Ga. In NE Brazil, the main Pan-African suture is probably buried beneath the Parnaíba Basin. The Transbrasiliano Lineament, interpreted as the prolongation of the Kandi–4°50 Lineament in Hoggar, may represent a cryptic suture.
West Gondwana: Pre-cenozoic correlations across the south atlantic region

hal-00412234
https://hal.archives-ouvertes.fr/hal-00412234
DOI : 10.1144/SP294.4

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
Although magmatism may occur during the earliest stages of continental rifting, its role in strain accommodation remains weakly constrained by largely 2-D studies. We analyze seismicity data from a 13 month, 39-station broadband seismic array to determine the role of magma intrusion on state-of-stress and strain localization, and their along-strike variations. Precise earthquake locations using cluster analyses and a new 3-D velocity model reveal lower crustal earthquakes beneath the central basins and along projections of steep border faults that degas CO2. Seismicity forms several disks interpreted as sills at 6-10 km below a monogenetic cone field. The sills overlie a lower crustal magma chamber that may feed eruptions at Oldoinyo Lengai volcano. After determining a new ML scaling relation, we determine a b-value of 0.87±0.03. Focal mechanisms for 65 earthquakes, and 13 from a catalogue prior to our array reveal an along-axis stress rotation of ∼60° in the magmatically active zone. New and prior mechanisms show predominantly normal slip along steep nodal planes, with extension directions ∼N90°E north and south of an active volcanic chain consistent with geodetic data, and ∼N150°E in the volcanic chain. The stress rotation facilitates strain transfer from border fault systems, the locus of early-stage deformation, to the zone of magma intrusion in the central rift. Our seismic, structural, and geochemistry results indicate that frequent lower crustal earthquakes are promoted by elevated pore pressures from volatile degassing along border faults, and hydraulic fracture around the margins of magma bodies. Results indicate that earthquakes are largely driven by stress state around inflating magma bodies.
ISSN: 1525-2027

hal-01667198
https://hal.archives-ouvertes.fr/hal-01667198
DOI : 10.1002/2017GC007027

Éditeur(s) : HAL CCSD Museum National d'Histoire Naturelle Paris
Résumé : This study focuses on new fossil faunas of bats discovered in North Africa following several field campaigns. The fossiliferous localities include those from the Early to Middle Eocene of Tunisia (Chambi) and Algeria (Glib Zegdou). Systematic and cladistic analyses carried out on the fossil material, primarily including isolated teeth, allow us to highlight the modalities of the radiation of the first modern microbats. These new faunas include eight well-identified new taxa belonging to five modern families: one Necromantidae (?Necromantis fragmentum Ravel, n. sp.), two Hipposideridae Miller, 1907 (?Palaeophyllophora tunisiensis Ravel, n. sp. and Hipposideros [Pseudorhinolophus] africanum Ravel, n. sp.), three Emballonuridae Gervais in de Castelnau, 1855 (Vespertiliavus kasserinensis Ravel, n. sp., ?Vespertiliavus aenigma Ravel, n. sp., and Pseudovespertiliavus parva Ravel n. gen., n. sp.), one Nycteridae (Khoufechia gunnelli Ravel n. gen., n. sp.) and an undetermined Vespertilionidae. Two other taxa are identified (Chambinycteris pusilli Ravel n. gen., n. sp. and Drakonycteris glibzegdouensis Ravel n. gen., n. sp.), but they show an original dental pattern which precludes a family attribution. Two cladistic analyses allow to clarify the phylogenetic position of the best documented taxa. The results highlight for Hipposideridae and Emballonuridae chiropterans a major dispersal axis from North Africa towards South Europe during the Middle Eocene.
ISSN: 1280-9659

hal-01467508
https://hal.archives-ouvertes.fr/hal-01467508
DOI : 10.5252/g2016n3a3

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
Rifting in a cratonic lithosphere is strongly controlled by several interacting processes including crust/mantle rheology, magmatism, inherited structure and stress regime. In order to better understand how these physical parameters interact, a 2 yr long seismological experiment has been carried out in the North Tanzanian Divergence (NTD), at the southern tip of the eastern magmatic branch of the East African rift, where the southward-propagating continental rift is at its earliest stage. We analyse teleseismic data from 38 broad-band stations ca. 25 km spaced and present here results from their receiver function (RF) analysis. The crustal thickness and Vp/Vs ratio are retrieved over a ca. 200 × 200 km2 area encompassing the South Kenya magmatic rift, the NTD and the Ngorongoro-Kilimanjaro transverse volcanic chain. Cratonic nature of the lithosphere is clearly evinced through thick (up to ca. 40 km) homogeneous crust beneath the rift shoulders. Where rifting is present, Moho rises up to 27 km depth and the crust is strongly layered with clear velocity contrasts in the RF signal. The Vp/Vs ratio reaches its highest values (ca. 1.9) beneath volcanic edifices location and thinner crust, advocating for melting within the crust. We also clearly identify two major low-velocity zones (LVZs) within the NTD, one in the lower crust and the second in the upper part of the mantle. The first one starts at 15–18 km depth and correlates well with recent tomographic models. This LVZ does not always coexist with high Vp/Vs ratio, pleading for a supplementary source of velocity decrease, such as temperature or composition. At a greater depth of ca. 60 km, a mid-lithospheric discontinuity roughly mimics the step-like and symmetrically outward-dipping geometry of the Moho but with a more slanting direction (NE–SW) compared to the NS rift. By comparison with synthetic RF, we estimate the associated velocity reduction to be 8–9 per cent. We relate this interface to melt ponding, possibly favouring here deformation process such as grain-boundary sliding (EAGBS) due to lithospheric strain. Its geometry might have been controlled by inherited lithospheric fabrics and heterogeneous upper mantle structure. We evidence that crustal and mantle magmatic processes represent first order mechanisms to ease and locate the deformation during the first stage of a cratonic lithospheric breakup.
ISSN: 0956-540X

hal-01622078
https://hal.archives-ouvertes.fr/hal-01622078
https://hal.archives-ouvertes.fr/hal-01622078/document
https://hal.archives-ouvertes.fr/hal-01622078/file/plasmanGJI2017.pdf
DOI : 10.1093/gji/ggx177