Systematics of Senecio sect. Crociseris (Compositae, Senecioneae)

Se revisa taxonómicamente Senecio sect. Crociseris (Compositae, Senecioneae),una de las cuatro principales secciones del género en el ámbito de Eurasia y el norte de África. Este grupo comprende hierbas rizomatosas, distribuidas principalmente del oeste de Europa y noroeste de África al oeste asiático, y presenta la mayor diversidad en el Mediterráneo septentrional. El nuevo tratamiento taxonómico que se propone reconoce 28 especies y 8 subespecies. Se ha hecho un especial esfuerzo en el análisis de la variabilidad del gr. S. doronicum, cuya sistemática ha sido objeto de controversia durante mucho tiempo. En este grupo se aceptan tres especies: S. doronicum, S.lagascanus, y S. provincialis, la primera con tres subespecies: subsp. doronicum, subsp.longifolius, y subsp. orientalis. Con el objetivo de indagar en las relaciones de las especies dentro de la sección y de ésta con otros grupos de Senecio, se han llevado a cabo análisis filogenéticos basados en secuencias ITS y de cloroplasto. Los resultados sugieren que la sect. Crociseris es un grupo parafilético, ya que incluye las especies secuenciadas de la sect. Doria. Además, complejos patrones de algunas secuencias ITS sugieren eventos de hibridación. Como resultado del estudio taxonómico se proponen las siguientes combinaciones: Senecio doronicum subsp. longifolius(Willk.) J. Calvo, Senecio doronicum subsp. orientalis (Ten.) J. Calvo, Senecio macedonicus subsp. barckhausiaefolius (Boiss. & Heldr.) J. Calvo, y Senecio racemosus subsp. kirghisicus(DC.) J. Calvo. Por otro lado, S. ruthenensis de Francia y S. lusitanicus de Portugal han sido sinonimizados a S. lagascanus, así como S. ovatifolius, S. pisidicus y S. tmoleus de Anatolia a S. kolenatianus, S. olympicus, y S. castagneanus respectivamente, S.bertramii de Líbano a S. cilicius, y S. delbesianus de Siria a S. racemosus subsp. racemosus. Se han lectotipificado setenta y cinco nombres, y neotipificado S. pyrenaicus y S. scopolii. Senecio gerardi Godr., S. doronicum (L.) L. y S. paucifolius S.G. Gmel. se propusieron a conservar. Se incluyen claves de identificación, descripciones detalladas, mapas de distribución e ilustraciones. Nueve táxones han sido ilustrados por primera vez.

Evidence from molecular systematics for decreased avian diversification in the pleistocene Epoch.

Pleistocene glaciations have been suggested as major events influencing speciation rates in vertebrates. Avian paleontological studies suggest that most extant species evolved in the Pleistocene Epoch and that species' durations decreased through the Pleistocene because of heightened speciation rates. Molecular systematic studies provide another data base for testing these predictions. In particular, rates of diversification can be determined from molecular phylogenetic trees. For example, an increasing rate of speciation (but constant extinction) requires shorter intervals between successive speciation events on a phylogenetic tree. Examination of the cumulative distribution of reconstructed speciation events in mtDNA phylogenies of 11 avian genera, however, reveals longer intervals between successive speciation events as the present time is approached, suggesting a decrease in net diversification rate through the Pleistocene Epoch. Thus, molecular systematic studies do not indicate a pulse of Pleistocene diversification in passerine birds but suggest, instead, that diversification rates were lower in the Pleistocene than for the preceding period. Documented habitat shifts likely led to the decreased rate of diversification, although from molecular evidence we cannot discern whether speciation rates decreased or extinction rates increased.

Vertebrate ecology and systematics : a tribute to Henry S. Fitch / edited by Richard A. Seigel ... [et al.].

no.10 (1984)

Systematics and zoogeography of Philippine amphibia.

v.33:no.4(1954)

Rb-Sr systematics of volcanic rocks and alteration minerals of ODP Hole 104-642E

Subaerially erupted tholeiites at Hole 642E were never exposed to the high-temperature seawater circulation and alteration conditions that are found at subaqueous ridges. Alteration of Site 642 rocks is therefore the product of the interaction of rocks and fluids at low temperatures. The alteration mineralogy can thus be used to provide information on the geochemical effects of low temperature circulation of seawater. Rubidium-strontium systematics of leached and unleached tholeiites and underlying, continentally-derived dacites reflect interactions with seawater in fractures and vesicular flow tops. The secondary mineral assemblage in the tholeiites consists mainly of smectite, accompanied in a few flows by the assemblage celadonite + calcite (+/- native Cu). Textural relationships suggest that smectites formed early and that celadonite + calcite, which are at least in part cogenetic, formed later than and partially at the expense of smectite. Smectite precipitation occurred under variable, but generally low, water/rock conditions. The smectites contain much lower concentrations of alkali elements than has been reported in seafloor basalts, and sequentially leached fractions of smectite contain Sr that has not achieved isotopic equilibrium. 87Sr/86Sr results of the leaching experiments suggest that Sr was mostly derived from seawater during early periods of smectite precipitation. The basalt-like 87Sr/86Sr of the most readily exchangeable fraction seems to suggest a late period of exposure to very low water /rock. Smectite formation may have primarily occurred in the interval between the nearly 58-Ma age given by the lower series dacites and the 54.5 +/- 0.2 Ma model age given by a celadonite from the top of the tholeiitic section. The 54.5 +/- 0.2 Ma Rb-Sr model age may be recording the timing of foundering of the Voring Plateau. Celadonites precipitated in flows below the top of the tholeiitic section define a Rb-Sr isochron with a slope corresponding to an age of 24.3 +/- 0.4 Ma. This isochron may be reflecting mixing effects due to long-term chemical interaction between seawater and basalts, in which case the age provides only a minimum for the timing of late alteration. Alternatively, inferrential arguments can be made that the 24.3 +/- 0.4 isochron age reflects the timing of the late Oligocene-early Miocene erosional event that affected the Norwegian-Greenland Sea. Correlation of 87Sr/86Sr and 1/Sr in calcites results in a two-component mixing model for late alteration products. One end-member of the mixing trend is Eocene or younger seawater. Strontium from the nonradiogenic endmember can not, however, have been derived directly from the basalts. Rather, the data suggest that Sr in the calcites is a mixture of Sr derived from seawater and from pre-existing smectites. For Site 642, the reaction involved can be generalized as smectite + seawater ++ celadonite + calcite. The geochemical effects of this reaction include net gains of K and CO2 by the secondary mineral assemblage. The gross similarity of the reactions involved in late, low-temperature alteration at Site 642 to those observed in other sea floor basalts suggests that the transfer of K and C02 to the crust during low-temperature seawater-ocean crust interactions may be significant in calculations of global fluxes.