Oidiopsis taurica : nuevo patógeno de pimiento (Capsicum annum L.) y ají (Capsicum frutescens L.) en Mendoza (Argentina)

En febrero de 1998 se observó en cultivos de pimiento y ají de Mendoza (Argentina) muerte anticipada de plantas con severos daños en la producción. La magnitud del problema motivó una prospección en los principales oasis de la provincia, a fin de describir la sintomatología, conocer su dispersión, estimar los daños causados y recolectar material para realizar estudios en laboratorio tendientes a confirmar su etiología. Se constató que la afección se encontraba distribuida en todos los oasis del centro y norte. La sintomatología en hojas se caracterizó por la presencia en la cara adaxial de manchas amarillentas, de forma circular de 15 a 20 mm de diámetro, con puntuaciones necróticas, con tendencia a presentarse en anillos concéntricos. En la cara abaxial, generalmente las lesiones eran acompañadas de un micelio blanco tenue. Posteriormente siguió una severa defoliación. La producción disminuyó notablemente y además en pimiento los frutos fueron afectados por escaldaduras de sol y perdieron su valor comercial. A partir de aislamientos de pimiento y ají, mantenidos en plantas de brincos (Impatiens balsamina L.), se inocularon plantas sanas y se logró reproducir la enfermedad en condiciones de invernáculo.

Physalis viscosa : un nuevo hospedero de Leveillula taurica en Argentina

Leveillula taurica (Lév.) Salm. es un hongo patógeno que se encuentra actualmente en expansión en nuestro país y en particular en la provincia de Mendoza. Physalis viscosa (camambú) es una especie muy difundida en Argentina. La misma es principalmente una maleza que crece espontáneamente en numerosos cultivos de interés económico y en sus alrededores. El hallazgo de L. taurica sobre una especie tan difundida fue el motivo de su estudio. Los síntomas característicos observados fueron parches cuneiformes amarillos en la cara adaxial de las hojas y en correspondencia con los mismos, en la abaxial se presentó un afelpado blanquecino formado por las fructificaciones asexuales del patógeno. El estudio etiológico realizado mediante la histopatología de los órganos afectados y la morfometría del patógeno confirmó la presencia del hongo parásito obligado Leveillula taurica (Lév.) Salm., en su forma anamórfica Oidiopsis taurica Sal. [= Oidiopsis sicula (Scal)]. La enfermedad en el camambú se ha difundido en forma importante en la provincia de Mendoza desde su primer hallazgo en el departamento de Tupungato en 1996. Se encuentra presente desde diciembre hasta mayo. Este prolongado período puede representar una importante fuente de inóculo para cultivos susceptibles al patógeno. La presente constituye la primera cita, no sólo a nivel nacional sino también mundial, de L. taurica sobre Physalis viscosa.

Oidiopsis haplophylli (Leveilula taurica): um patógeno polífago e amplamente distribuído no Brasil.

2005

Oidiopsis (Erysiphaceae) on Euphorbia spp. in Australia and Vanuatu

One specimen of powdery mildew on Euphorbia cyathophora from Vanuatu and 11 specimens on E. cyathophora, E. dentata, E. heterophylla and E. leucocephala from Australia were studied. All were shown to represent the Oidiopsis anamorph of Leveillula taurica, which is described. This is the first record of Oidiopsis in Vanuatu. E. leucocephala is a new host record for this powdery mildew.

Powdery mildew on Passiflora in Australia

Oidiopsis sp., the anamorph of Leveillula taurica (Erysiphaceae), is reported for the first time in Australia on Passiflora edulis, and Oidium passiflorae on Passiflora foetida. A detailed description and illustration of the specimens are given.

Control of Leveillula taurica in tomato by Acremonium alternatum is by induction of resistance, not Hyperparasitism

Spores of the hyperparasite Acremonium alternatum reduced powdery mildew infection by Leveillula taurica on greenhouse tomato. The effect was slightly increased when spores were applied killed, and therefore not due to direct parasitism. The effect was systemic, protecting untreated leaves above the treated ones. Spores killed by heat had more effect than when killed by UV, so the effect was presumably due to induction of host resistance by substances released when cells were heat killed. The size of the effect depended upon leaf age and level of infection. Effects on primary infection and expansion of successful infections appear to be under independent control.

Flora taurico-caucasica exhibens stirpes phaenogamas in Chersoneso Taurica et regionibus caucasicis sponte crescentes /

Contiene: T. 1 - T. 2 - Supplementum.

Euripidis Iphigenia Taurica.

p. [v]-vi follows p. vii-viii; p. ix-x follows xi-xii; p. xiii-xiv follows p. xv-xvi.

Taxonomic notes on two powdery mildews: Phyllactinia chorisiae and Ovulariopsis wissadulae (Erysiphaceae: Phyllactinieae)

The powdery mildew Phyllactinia chorisiae has been considered conspecific with P. guttata. A re-examination of the type material of P. chorisiae and another specimen showed that this fungus, unlike P. guttata, has dimorphic conidia and its anamorph does not belong to the genus Ovulariopsis, which is the typical anamorph for Phyllactinia species. This suggests that P. chorisiae is morphologically distinct from P. guttata and should no longer be accepted as a synonym. Re-evaluation of type material of Oidiopsis wissadulae revealed that it has monomorphic conidia (mostly lemon-shaped) and hemiendophytic mycelium, a combination of characters that clearly places this fungus in the genus Ovulariopsis. Emended descriptions of P. chorisiae and Ovulariopsis wissadulae are presented.

Leaf-clearing and staining techniques for the observation of conidiophores in the Phyllactinioideae (Erysiphaceae)

Some whole leaf-clearing and staining techniques are described for the microscopic observation of the origin of powdery mildew conidiophores, whether from external mycelium or internal mycelium, emerging through stomata. These techniques enable separation of the two genera, Oidiopsis and Streptopodium, in the Erysiphaceae.

Studi sull'immaginario musicale in Euripide

La dissertazione è suddivisa in due capitoli più tre appendici. Nel I capitolo, Musica e dolore, si indagano i casi di metamusicalità in riferimento al dolore, che si intensificano in Euripide: si nota lo sviluppo di una riflessione sul ruolo della mousike rispetto al dolore, espressa attraverso un lessico medico e musicale. Si dimostra che in Euripide si pone il problema di quale scopo abbia la musica, se sia utile, e in quale forma lo sia. Nella prima produzione si teorizza una mousa del lamento come dolce o terapeutica per chi soffre. Molti personaggi, però, mostrano sfiducia nel potere curativo del lamento. Nell’ultima produzione si intensificano gli interrogativi sulla performance del canto, che si connotano come casi metamusicali e metateatrali. Nell’Elena, nell’Ipsipile e nelle Baccanti, E. sembra proporre una terapia ‘omeopatica’ del dolore attraverso la musica orgiastico-dionisiaca. Nel II capitolo, Natura e musica, si sceglie l’Ifigenia Taurica come esempio di mimetismo orchestico-musicale fondato – oltre che su casi di autoreferenzialità – su un immaginario naturale che, ‘facendo musica’, contribuisce all’espressività della choreia e della musica in scena. Si ipotizza inoltre un accompagnamento musicale mimetico rispetto ai suoni della natura e movimenti di danza lineari accanto a formazioni circolari, che sembrano richiamare la ‘doppia natura’ del ditirambo. L’Appendice I, Gli aggettivi poetici ξουθός e ξουθόπτερος: il loro significato e la loro potenzialità allusiva, affronta un caso particolare e problematico di ‘mimetismo lessicale’, innescato dal termine ξουθός e dal composto euripideo ξουθόπτερος. Si dimostra che l’aggettivo indica originariamente un movimento vibratorio, ma sviluppa anche un senso sonoro, ed è quindi un termine evocativo rispetto alla performance. Nell’Appendice II, Il lessico musicale in Euripide, è raccolto il lessico euripideo coreutico-musicale. Nell’Appendice III, La mousike nei drammi euripidei, sono raccolti i riferimenti alla mousike in ogni dramma.

Chemobiostratigraphy of the Cretaceous/Paleocene boundary at ODP Hole 120-750A

An integrated biostratigraphic and stable isotope investigation was conducted on a high-latitude sequence across the Cretaceous/Paleogene (K/P) boundary recovered in Hole 750A in the southern Indian Ocean. The sequence consists of nannofossil chalk and is discontinuous across the boundary; missing is an estimated 0.3-m.y. late Maestrichtian and early Danian interval. Nonetheless, because calcareous nannofossil Zones NP1 and NP2 are well-developed, micropaleontological studies of the sequence have yielded a detailed record of Danian high-latitude microplankton evolution. In addition, stable carbon isotope analyses of planktonic and benthic foraminifer and bulk samples provide a record of late Maestrichtian and early Danian surface- and deep-water carbon isotope variations. Together, the carbon isotope and carbonate accumulation records serve as an index of regional marine net productivity across the boundary. Earliest Danian nannoplankton assemblages consisted mainly of persistent genera that were generally rare or absent in the Upper Cretaceous at Hole 750A. However, by 0.5-0.6 m.y. after the boundary, newly evolving Danian taxa became dominant. The turnover in nannofossil assemblages was accompanied by significant changes in rates of net productivity as gauged by carbon isotope distributions and carbonate accumulation rates. During the period dominated by persistent taxa, net productivity was extremely low, as reflected by the absence of vertical delta13C gradients and reduced carbonate accumulation rates. Later in the Danian, as new species evolved and flourished, vertical delta13C gradients reappeared and carbonate accumulation rates increased, signaling partial recovery of net productivity in this region. The absolute timing and magnitude of late Maestrichtian and early Danian biotic and geochemical changes in the southern Indian Ocean were similar to those recorded in other pelagic K/P boundary sequences from low- and mid-latitude Atlantic and Pacific sites, indicating that these events were ubiquitous.

Planktic foraminiferal assemblage turnover at the Cretaceous-Tertiary boundary

Three uppermost Cretaceous through basal Paleocene stratigraphic sequences are examined for planktic foraminiferal assemblage stability and temporal succession patterns. These sequences are at mid-latitude South Atlantic DSDP Site 528, then-equatorial Pacific DSDP Site 577 and the Tethyan shelf Ben Gurion section of the Negev, Israel. In order to better estimate biogeographic patterns and habitat preferences, the results of these analyses are compared to previous Cretaceous biogeographic studies and to previous analyses of Cretaceous-Tertiary (K/T) boundary shelf and epicontinental sections. Results indicate that immediately following the K/T boundary, the examined epicontinental and open-ocean sites were exploited primarily by previously epicontinental planktic foraminiferal assemblages. This pattern of K/T boundary assemblage dominance suggests the geologically instantaneous break-down of Late Cretaceous epicontinental and open-ocean biogeographic provincialization. This shift in open-ocean foraminiferal assemblages is not consistent with models of nonselective K/T boundary extinctions, but is consistent with models of extinction resistence and offshore expansion of nearshore taxa. The re-establishment of stable biogeographic differences between open-ocean and epicontinental planktic foraminiferal assemblages occurs by the basal Parvularugoglobigerina eugubina Zone. At open-ocean sites 528 and 577 and the outershelf Ben Gurion section, P0 and P. eugubina Zone faunal records are marked by a pronounced alternation between Paleocene biserial- and non-biserial-dominated assemblages, This alternation appears strongly damped at shelf and epicontinental sections previously examined. The first appearance and peak magnitude of abundant earliest Paleocene trochospiral forms (Parvularugoglobigerina, Eoglobigerina, Morozovella, Globoconusa) also vary from site to site and may depend closely on levels of primary carbonate productivity.