Evaluation de la qualité des zones de production conchylicole - Département d'Ille et Vilaine - Edition 2016

Après un rappel des objectifs, du fonctionnement et de la méthode d’interprétation des résultats du réseau de contrôle microbiologique des zones de production conchylicoles (REMI) et du réseau d’observation de la contamination chimique (ROCCH), ce rapport inclut un bilan national et décrit le programme annuel du département de l’Ille-et-Vilaine (35). Il présente l’ensemble des résultats obtenus, en particulier l’estimation de la qualité microbiologique et chimique des zones de production de coquillages classées. Pour la deuxième année consécutive, les résultats du suivi microbiologique sont globalement bons dans le département d’Ille-et-Vilaine. Les alertes ont été également très peu nombreuses, une seule alerte en centre Rance en 2015 est recensée. L’estimation de la qualité sanitaire s’améliore en 2015 pour quelques sites. Par exemple en baie du Mont Saint- Michel où trois zones sont estimées de bonne qualité. Mais les résultats de l’année 2013 pénalisent encore certaines zones conchylicoles, notamment en Rance et en baie de Saint-Malo ou la situation reste fragile. Cela concerne notamment deux zones estimées en très mauvaise qualité. Deux autres zones, en baie de Saint-Malo et dans l’estuaire de la Rance, actuellement classées B, ne disposent pas d’assez de données pour pouvoir estimer leur qualité. La récupération des échantillons provenant de ces zones est dépendante de la collaboration des pêcheurs. Une convention avec le CDPMEM 35 (Comité Départementale des Pêches Maritimes et des Elevages Marin d’Ille-et-Vilaine) a été signée en novembre 2015 pour améliorer la situation.

[Tracteur] Exelsior 35/40 HP [tractant une herse à] Rocquencourt, Versailles, 13/3/20 : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 58493

1.° Tractatus pacis inter Ludovicum IX. Regem Francorum, et Henricum III. Regem Angliae : anno 1259. — 2.° Tractatus pacis inter Philippum III. Regem Francorum, et Edwardum I. Regem Angliae : anno 1279. — 3.° Tractatus pacis inter eosdem Reges : anno 1286. — 4.° Quarta et ultima pax facta inter Reges : anno 1303. translata de romancio in latinum, de verbo ad verbum. — 5.° Alia concordantia, seu compositio vel pax inter Reges : anno 1303. — 6.° Pronunciatio Bonifacii, Papae, super pacibus : anno pontificatus quarto. — 7.° De remediis Aquitanorum adversùs vexationem curiae Regis Franciae. — 8.° Copia arresti contra Arnaldum de Romynhano, dati anno 1312. — 9.° Variae litterae Philippi Pulchri et Ludovici X. de rebus Anglicis. — 10.° Bulla Clementis, Papae V. approbans donationem Motae et domorum de Pessaco, factam ecclesiae Burdegalensi à nobili viro Gaillardo de Guto, germano suo, anno primo pontificatus. — 11.° Traitté de paix conclu entre les Rois Philippe et Edouard ; sans date. — 12.° Lettres de Charles IV. Roy de France et de Navarre, touchant les excès commis au lieu de Saint-Sacerdos par le Senechal de Gascogne : l'an 1324. — 13.° Traitté entre la France et l'Angleterre : en la même année. — 14.° Judicium latum apud Oleronem, anno 1287. per D. Norwicensem Episcopum, contra D. Joannem de Greilliaco, dudum Senescallum Vasconiae. — 15.° Tractatus matrimonii inter Alienoram filiam Edwardi Regis Angliae, et Alphonsum filium majorem Petri Regis Aragonum. — 16.° Litterae Petri, Regis Aragonum, de matrimonio filii sui Alphonsi cum Alienora, filia primogenita Regis Edwardi. — 17.° Joannis XXII. bulla contra Michaëlem de Cesena, Ministrum generalem ordinis Minorum : VIII. idus Junii, pontificatus anno XII. — 18.° Edwardi, Regis Anglorum, constitutiones variae ad Aquitaniam spectantes et ad Angliam. — 19.° Traitté de paix entre les Rois de France et d'Angleterre, fait en l'an 1325. — 20.° Litterae Agennensium ad Carolum IV. Regem Franciae, pro Rege Angliae, nominatim de facto Sancti-Sacerdotis, scriptae anno 1324. — 21.° Tractatus matrimonii inter Alphonsum, Regem Castellae et Legionis, et Alienoram, filiam Edwardi Regis Angliae ; item alius inter Edwardum, Regis Angliae primogenitum, et Alienoram sororem Regis Castellae : anno 1325. — 22.° Instructions données par le Roy d'Angleterre à ses Ambassadeurs allans en Espagne pour le fait dudit mariage. — 23.° Abusiones quae exercentur in regno Angliae circa beneficia ecclesiastica ; et remedia sine quibus nunquam cessare creduntur. — 24.° Clementis V. bulla de saecularisatione monasterii de sancto Aemiliano, in dioecesi Burdigalensi ; data anno pontificatus quinto. — 25.° Litterae Edwardi II. Regis Angliae, de servanda pace facta cum Carolo IV. Rege Franciae. — 26.° Ejusdem litterae quibus Edmundum, Comitem Cantiae, fratrem suum, constituit Capitaneum in Ducatu Aquitaniae. — 27.° Lettres de Charles IV. Roy de France, contre le Roy d'Angleterre, qui refusoit de luy faire les foy et hommage pour la Duché d'Aquitaine : de l'année 1324. — 28.° Litterae ejusdem Caroli IV. Regis Francorum, de eadem re ; quibus Carolo, Comiti Valesiae, patruo suo, dat potestatem puniendi rebelles Aquitaniae ; datae anno 1324. — 29.° Litterae ejusdem de salvagardia Guillelmi Galteri, Clerici, datae anno 1323. — 30.° Ejusdem litterae pro Margareta de Guouda, tutrice Pontii domini de Castellione, filii sui, datae anno 1323. — 31.° Ejusdem litterae pro Comitissa Fuxi et Vicecomitissa Bearni et Marciani, tutrice Gastonis filii sui ; datae anno 1322. — 32.° Litterae Antonini Pessaigne, Senescalli Ducatus Aquitaniae, quibus Ostencium Jordani, Clericum ac Jurisperitum, constituit suum et Regis Angliae Procuratorem ; datae anno 1318. — 33.° Litterae Almarici domini de Credonio, Senescalli Ducatus Aquitaniae, quibus Roberto de la Vertadausa, Anglico, decem libras Turonensium parvorum singulis annis solvendas concedit vice et nomine Regis Angliae ; datae anno 1322. — 34.° Divers actes entre les Rois de France et d'Angleterre, pour assurer la paix ; faits depuis l'an 1259. jusques en 1323. — 35.° Acta processus habiti in curia Romana inter capitulum ecclesiae Coventrensis et capitulum ecclesiae Lichefeldiensis de electione Episcopi, tempore Joannis XXII. — 36.° Traitté d'alliance et de confederation entre la France et l'Ecosse contre l'Angleterre ; fait en 1325. — 37.° Articuli exhibiti à Procuratore ecclesiae Lichfeldensis. — 38.° Articuli exhibiti à Procuratore ecclesiae Coventrensis. — 39.° Joannis XXII. bulla de unione Episcopatuum Corkagiensis et Clonensis, data Avenione anno pontificatus XI. — 40.° Acta processus apud eumdem Papam agitati super praebenda sancti Stephani in ecclesia Beverlacensi.

Colbertinus

Cahier contenant des notes, en turc, en persan, en arabe, dont les plus importantes sont (folio 6 verso) des fetvas relatifs aux biens de main-morte de Sainte-Sophie, et le commencement d'un traité d'Insha (folio 35 verso).

Ravius (Christiani Ravij Berlinatis) ; Thévenot.

Recueil de poésies, par « HENRY BAULDE » (fol. 30, 32, 35, 36, 37, 39, 40, 43, 44, 46, 47, 56, 59, 60, 61, 65, 68, 69, 70, 73, 74), « ALAIN CHARRETIER » (fol. 15), « JEHAN DAUTON » (fol. 9), « JEHAN MAROT » (fol. 29, 30), « JEHAN MOLINET » (fol. 77, 85, 90, 93, 94, 95) et « JEHAN ROBERTET » (fol. 1, 75).

Commençant par : « Estant couché soubz ung myrthe plaisant, Et maintz chasteaulx en Espaigne faisant... » et finissant par : « Sans parage ou riens n'est nect, Moulu d'un groz Moulinet. Fin de la complaincte de Grece, composée par le dict Molinet » .

Musée littéraire : choix de littérature contemporaine française et étrangère. Série 35

Collection : Le siècle ; 1-46

Bulletin de la Commission historique du Département du Nord.

Mode of access: Internet.

A comparison of the hazard perception ability of matched groups of healthy drivers aged 35 to 55, 65 to 74, and 75 to 84 years

We examined differences in response latencies obtained during a validated video-based hazard perception driving test between three healthy, community-dwelling groups: 22 mid-aged (35-55 years), 34 young-old (65-74 years), and 23 old-old (75-84 years) current drivers, matched for gender, education level, and vocabulary. We found no significant difference in performance between mid-aged and young-old groups, but the old-old group was significantly slower than the other two groups. The differences between the old-old group and the other groups combined were independently mediated by useful field of view (UFOV), contrast sensitivity, and simple reaction time measures. Given that hazard perception latency has been linked with increased crash risk, these results are consistent with the idea that increased crash risk in older adults could be a function of poorer hazard perception, though this decline does not appear to manifest until age 75+ in healthy drivers.

Disclosure under the prescribed insurance contracts regime : Section 35 of the Insurance Contracts Act 1984 and consumer protection revisited

Section 35 of the Insurance Contracts Act 1984 requires insurers offering insurance policies in six prescribed areas "to clearly inform" prospective insureds of any departure their policies may constitute from the standard covers established by the Act and its accompanying Regulations. This prescribed insurance contracts regime was designed to remedy comprehension problems generated by the length and complexity of insurance documents and to alleviate misunderstanding over the terms and conditions of individual policies. This article examines the rationale underpinning s 35 and the prescribed insurance contracts regime and looks at the operation of the legislation with particular reference to home contents insurance in Australia. It is argued that the means whereby disclosure of derogation from standard cover may be effected largely negates the thrust of the prescribed insurance contract reform. Recommendations to address these operational deficiencies are made.

Climate variability over the last 35,000 years recorded in marine and terrestrial archives in the Australian region : an OZ-INTIMATE compilation

The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regional climate variability both today and during the Late Quaternary. A synthesis of marine and terrestrial climate records, combining findings from the Southern Ocean, temperate, tropical and arid zones, identifies a complex response of climate proxies to a background of changing boundary conditions over the last 35,000 years. Climate drivers include the seasonal timing of insolation, greenhouse gas content of the atmosphere, sea level rise and ocean and atmospheric circulation changes. Our compilation finds few climatic events that could be used to construct a climate event stratigraphy for the entire region, limiting the usefulness of this approach. Instead we have taken a spatial approach, looking to discern the patterns of change across the continent. The data identify the clearest and most synchronous climatic response at the time of the Last Glacial Maximum (LGM) (21 ± 3 ka), with unambiguous cooling recorded in the ocean, and evidence of glaciation in the highlands of tropical New Guinea, southeast Australia and Tasmania. Many terrestrial records suggest drier conditions, but with the timing of inferred snowmelt, and changes to the rainfall/runoff relationships, driving higher river discharge at the LGM. In contrast, the deglaciation is a time of considerable south-east to north-west variation across the region. Warming was underway in all regions by 17 ka. Post-glacial sea level rise and its associated regional impacts have played an important role in determining the magnitude and timing of climate response in the north-west of the continent in contrast to the southern latitudes. No evidence for cooling during the Younger Dryas chronozone is evident in the region, but the Antarctic cold reversal clearly occurs south of Australia. The Holocene period is a time of considerable climate variability associated with an intense monsoon in the tropics early in the Holocene, giving way to a weakened monsoon and an increasingly El Niño-dominated ENSO to the present. The influence of ENSO is evident throughout the southeast of Australia, but not the southwest. This climate history provides a template from which to assess the regionality of climate events across Australia and make comparisons beyond our region. The data identify the clearest and most synchronous climatic response at the time of the Last Glacial Maximum (LGM) (21 ± 3 ka), with unambiguous cooling recorded in the ocean, and evidence of glaciation in the highlands of tropical New Guinea, southeast Australia and Tasmania. Many terrestrial records suggest drier conditions, but with the timing of inferred snowmelt, and changes to the rainfall/runoff relationships, driving higher river discharge at the LGM. In contrast, the deglaciation is a time of considerable south-east to north-west variation across the region. Warming was underway in all regions by 17 ka. Post-glacial sea level rise and its associated regional impacts have played an important role in determining the magnitude and timing of climate response in the north-west of the continent in contrast to the southern latitudes. No evidence for cooling during the Younger Dryas chronozone is evident in the region, but the Antarctic cold reversal clearly occurs south of Australia. The Holocene period is a time of considerable climate variability associated with an intense monsoon in the tropics early in the Holocene, giving way to a weakened monsoon and an increasingly El Niño-dominated ENSO to the present. The influence of ENSO is evident throughout the southeast of Australia, but not the southwest. This climate history provides a template from which to assess the regionality of climate events across Australia and make comparisons beyond our region.

Reply to the comments on “A study of the phosphate mineral kapundaite NaCa(Fe3+)4(PO4)4(OH)3·5(H2O) using SEM/EDX and vibrational spectroscopic methods” by Frost et al. (2014)

"The authors agree with the statements made by Mills and Christy on the study of kapundaite [1]. These authors are correct and have removed any confusion about the origin of the sample kapundaite. The authors (Frost et al.) confirm the sample of kapundaite studied in this work is from the Tom‘s quarry, Australia and can be considered a type material. The authors do not accept the statements by Mills and Christy on “type minerals”. The sample of kapundaite from the Australian source is from the collection of the Geology Department of the Federal University of Ouro Preto, Minas Gerais, Brazil with sample code SAC-111. At least if our mineral sample is not a co-type mineral, our sample is from the same origin as the type mineral. Samples..."--publisher website.