989 resultados para Insectivora, Fossil


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The description of Micropygomyia brandaoi, a new species of fossil phlebotomine sand fly, is based on one male specimen obtained from Dominican amber of the Miocene period (20 million years). In this new species, the fifth palpal segment is long, the coxite lacks a setal tuft and the style shows four well-developed spines. This set of characters allowed us to place the new species in the genus Micropygomyia Barretto.

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On a testé la sensibilité présumée aux basses températures de Suncus etruscus, le plus petit mammifère connu. Nourri à profusion, cette espèce a supporté des températures inférieures à 0° C. L'activité de l'animal (=absence du nid) à une température ambiante de 0-10° C s'élève en moyenne de 303min/24 h contre 358 min24 h à des températures de 15°-20° C. Si on retire toute nourriture à la musaraigne étrusque, celle-ci entre en hypothermie réversible et léthargique, de laquelle elle sort de temps en temps à la recherche de nourriture. En léthargie, la température corporelle est d'environ 2° C au dessus de la température ambiante. Avec 1 1/2 à 2 g de nourriture par jour et à la température ambiante de 16° à 18° C, les phases de léthargie durent de 1 1/2 à 2 h avec un maximum de 7 1/2h. En 24 h, un animal insuffisamment nourri montrait une activité totale de 205 min seulement. Pendant 696 min l'animal a dormi en conservant sa température "normale", et pendant 539 min il était en léthargie. L'hypothermie réversible chez un représentant des Soricidae s'explique probablement par une insuffisance de son métabolisme par rapport à sa taille minuscule. Comme les espèces du genre Sorex de taille voisine n'ont pas la possibilité d'entrer en léthargie réversible, cette adaptation particulière peut être considérée comme un indice d'un métabolisme relativement bas chez les Crocidurinae

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Le rythme journalier de l'activité a été étudié en captivité, à 25° C, chez 7 espèces de Crocidurinae africaines (Sylvisorex megalura, Crocidura bottegi, C. jouvenetae, C. poensis, C. wimmeri, C. flavescens, C. giffardi), pesant entre 4 et 100 g. Ces observations sont comparées à des données choisies obtenues à 5° C et 20° C chez deux espèces européennes (Suncus etruscus et Crocidura russula). 1. L'activité journalière totale n'est pas liée de façon nette au poids corporel au sein des espèces étudiées. 2. Les espèces tropicales sont caractérisées par une activité presque exclusivement nocturne (4 à 30min/h de nuit contre 0 à 2 min/f de jour). Durant le repos diurne, C. jouvenetae présente régulièrement des torpeurs spontanées. 3. Les espèces européennes ont comparativement une activité diurne importante. En été, à température élevée, l'activité présente cependant également un rythme journalier marqué à prédominance nocturne; ce rythme s'atténue progressivement lorsque la température s'abaisse, essentiellement par la diminution de l'activité nocturne. Une faible activité diurne semble caractériser les Crocidurinae. Cette particularité est discutée à la lumière de données physiologiques et paléozoogéographiques.

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Some aspects of torpor have been studied among captive Suncus etruscus by recording the nest temperature. Torpors show a circadian pattern and occur spontaneously or can be induced by food shortage. Body temperature can be controlled during torpor, remaining relatively high at low ambiant temperatures. At 20° C, spontaneous torpors seem to be less deep than induced tropors, but both show similar patterns at 5-8 ° C. Spontaneous torpors begin between 01°° and 06°°, whereas the onset of diet induced torpors seems to depend also on food exhausting. The rates of activity (A) and of torpor (T) show under constant conditions a daily variability. Increase of T is linked with a decrease of A and the relationship could agree with A(%) = Ao( 1-T/100), where Ao is daily rate of activity when T = 0. Occurence of torpor among other Soricidae, possible occurence among free living Suncus etruscus and energy saving are discussed

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As the morphological determination of living individuals of the two sibling species S. araneus and S. coronatus is not possible, we have tested two biochemical methods to determine these shrews in ecological studies. After producing specific antibodies by rabbits, we performed an immunological test on 25 individuals. With this first method, a correct determination was achieved in 76% of the cases only. The second method proved very successful: a polyacrylamide gel electrophoresis showed a systematic difference for albumin (73 individuals analyzed). According to our experience, the necessary blood sampling (10-20 μl) seems harmless for the shrews

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Microsatellites are used to unravel the fine-scale genetic structure of a hybrid zone between chromosome races Valais and Cordon of the common shrew (Sorex araneus) located in the French Alps. A total of 269 individuals collected between 1992 and 1995 was typed for seven microsatellite loci. A modified version of the classical multiple correspondence analysis is carried out. This analysis clearly shows the dichotomy between the two races. Several approaches are used to study genetic structuring. Gene flow is clearly reduced between these chromosome races and is estimated at one migrant every two generations using X-statistics and one migrant per generation using F-statistics. Hierarchical F- and R-statistics are compared and their efficiency to detect inter- and intraracial patterns of divergence is discussed. Within-race genetic structuring is significant, but remains weak. F-ST displays similar values on both sides of the hybrid zone, although no environmental barriers are found on the Cordon side, whereas the Valais side is divided by several mountain rivers. We introduce the exact G-test to microsatellite data which proved to be a powerful test to detect genetic differentiation within as well as among races. The genetic background of karyotypic hybrids was compared with the genetic background of pure parental forms using a CRT-MCA. Our results indicate that, without knowledge of the karyotypes, we would not have been able to distinguish these hybrids from karyotypically pure samples.

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Controlled interbreedings were performed between distinct chromosomal races or forms of Sorex araneus coming from populations of Swiss and French Alps. Four mating pairs including homozygous individuals of the Vaud race, the Valais race, the Intermediate Vaud-Acrocentric form and the Acrocentric form have led to several heterozygous hybrid litters. The karyotypes of the parents were determined from cultures of cartilaginous cells. The karyotypes of the offsprings were determined with a classical method. The production of hybrids between different races suggests the absence of postmating barrier between the Vaud race and the Intermediate form, the Acrocentric form and the Intermediate form, the Acrocentric form and the Valais race.

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Comprend : Description of fossil radiolaria from the rocks of Central Borneo, obtained by prof. Dr. G. A. F. Molengraaff in the dutch exploring expedition of 1893-94

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The following study should clear up the structures of the H-shaped profile found in the hairs of some shrews and show if it has a taxonomic signification. Therefore we studied the concerned hair structures by scanning electron microscopy in 8 genera. The special hair-shape, which is confined to the terminal segment of guard hairs, is found in the species of the following genera:Sorex, Neomys, Blarina andCryptotis, all members of the subfamily Soricinae. All the examined members of the subfamily Crocidurinae, i.e.Crocidura, Praesorex, Suncus andSylvisorex show a simple hair shape. The H-shaped hair characterizes the Soricinae as a monophyletic unity. Yet, the morphological criteria of hair complete the osteological criteria of Repenning (1967) an plead for the validitiy of the often refuted subfamilies.

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Mineral dust aerosols recently collected at the high-altitude Jungfraujoch research station (46 degrees 33'51 `' N, 7 degrees 59'06 `' E; 3580 m a.s.l.) were compared to mineral dust deposited at the Colle Gnifetti glacier (45 degrees 52'50 `' N, 7 degrees 52'33 `' E; 4455 m a.s.l.) over the last millennium. Radiogenic isotope signatures and backward trajectories analyses indicate that major dust sources are situated in the north-central to north-western part of the Saharan desert. Less radiogenic Sr isotopic compositions of PM10 aerosols and of mineral particles deposited during periods of low dust transfer likely result from the enhancement of the background chemically-weathered Saharan source. Saharan dust mobilization and transport were relatively reduced during the second part of the Little Ice Age (ca. 1690-1870) except within the greatest Saharan dust event deposited around 1770. After ca. 1870, sustained dust deposition suggests that increased mineral dust transport over the Alps during the last century could be due to stronger spring/summer North Atlantic southwesterlies and drier winters in North Africa. On the other hand, increasing carbonaceous particle emissions from fossil fuel combustion combined to a higher lead enrichment factor point to concomitant anthropogenic sources of particulate pollutants reaching high-altitude European glaciers during the last century.

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Previous morphological and cytological analyses have suggested that the arctic shrew (Sorex arcticus) as currently recognized may be two distinct species. Specifically, those studies demonstrated considerable differentiation between the putative subspecies S. a. maritimensis and one or both of the other two subspecies, S. a. arcticus and S. a. laricorum. Phylogenetic analysis of 546 base pairs of cytochrome b sequence data from 10 arctic shrews from across Canada indicates that maritimensis is the sister-group to arcticus + laricorum. Furthermore, there is considerable genetic divergence between maritimensis and the other two putative subspecies (similar to8-9%; Kimura's two-parameter distance). Given that maritimensis and arcticus + laricorum appear to be reciprocally monophyletic clades with considerable genetic divergence (i.e., greater than that between other recognized pairs of sister-species within the S. araneus-arcticus group), we propose that S. maritimensis be recognized as a distinct species. The proportion of third-position transversion substitutions between S. arcticus and S. maritimensis suggests that these two species shared a common ancestor approximately 2.4 million years ago.

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Despite the advancement of phylogenetic methods to estimate speciation and extinction rates, their power can be limited under variable rates, in particular for clades with high extinction rates and small number of extant species. Fossil data can provide a powerful alternative source of information to investigate diversification processes. Here, we present PyRate, a computer program to estimate speciation and extinction rates and their temporal dynamics from fossil occurrence data. The rates are inferred in a Bayesian framework and are comparable to those estimated from phylogenetic trees. We describe how PyRate can be used to explore different models of diversification. In addition to the diversification rates, it provides estimates of the parameters of the preservation process (fossilization and sampling) and the times of speciation and extinction of each species in the data set. Moreover, we develop a new birth-death model to correlate the variation of speciation/extinction rates with changes of a continuous trait. Finally, we demonstrate the use of Bayes factors for model selection and show how the posterior estimates of a PyRate analysis can be used to generate calibration densities for Bayesian molecular clock analysis. PyRate is an open-source command-line Python program available at http://sourceforge.net/projects/pyrate/.

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Biogeographic studies dealing with Bombyliidae are rare in the literature and no information is available on its origin and early diversification. In this study, we found evidence from molecular phylogeny and from fossil record supporting a Middle Jurassic origin of the Bombylioidea, taken as a starting point to discuss the biogeography and diversification of Crocidiinae. Based on a previously published phylogenetic hypothesis, we performed a Brooks Parsimony Analysis (BPA) to discuss the biogeographical history of Crocidiinae lineages. This subfamily is mostly distributed over arid areas of the early components of the Gondwanaland: Chile and southern Africa, but also in southwestern Palaearctic and southwestern Nearctic. The vicariant events affecting the Crocidiinae biogeography at the generic level seems to be related to the sequential separation of a Laurasian clade from a Gondwanan clade followed by the splitting of the latter into smaller components. This also leads to a hypothesis of origin of the Crocidiinae in the Middle Jurassic, the same period in which other bombyliid lineages are supposed to have arisen and irradiated.