A new infrageneric classification and phylogenetic trends in the genusRhododendron (Ericaceae)

Recent studies have improved the infrageneric classification ofRhododendron, including my own investigations on flavonoids and anthocyanins as chemosystematic markers. From a synoptical comparison of morphological, anatomical and phytochemical characters a new system for the genus is proposed. Phylogenetic character progressions and relationships among subgenera, sections and subsections are discussed and illustrated. Key positions for subg.Candidastrum between chori subgenerumRhododendron andNomazalea, and for subg.Choniastrum between chori subgenerumHymenanthes andNomazalea are suggested.     

葡萄属营养器官的比较解剖学及其系统学意义

本文对国产葡萄属24个种、6个变种和4个美洲种进行了比较解剖学研究。比较观察了茎、节、 叶柄、叶片的维管系统、厚角组织、厚壁组织、毛状体、后含物、叶表皮角质等解剖学特征。并讨论了它们在系统学上的意义。     

Das phylogenetische System der Tanaidacea und die Frage nach Alter and Herkunft der Crustaceenfauna des antarktischen Festlandsockels1,2

The phylogenetic system of the Tanaidacea and the question of age and origin of the crustacean fauna on the Antarctic shelf The final breakup of Gondwanaland during the Tertiary not only played an important role in establishing modern climates and oceanic currents but also had a tremendous influence on the composition of the Recent crustacean fauna. Analysis of the fossil record of the Tanaidacea shows that all Recent families had evolved before the Eocene. They all, therefore, had the chance to colonize the Antarctic shelf area. However, the tanaidacean fauna of this region is represented exclusively by phylogenetically young taxa. The species composition is atypical and does not correspond to those of other zoogeographic regions. Surprisingly, in the West Antarctic there occur some phylogenetic older taxa which are not recorded from the East Antarctic. In general, the species composition of the East Antarctic tanaidacean fauna is more like that of the deep sea while that of the West Antarctic is characterized by additional “littoral elements”. For the interpretation of recognized distribution patterns are most important geological events and the resulting effects on the changes in the world climates, e. g. it is commonly excepted that there is a continuous decrease of the surface water temperature since the paleocene. Deduced from foraminiferan data, it can be assumed that almost the entire Antarctic tanaidacean fauna was extinguished during the first dramatic drop of temperature. Cold-stenothermic eurybathic species then have colonized the Antarctic shelf. After the phase of maximal glaciation in the Pliozene the fauna of the West Antarctic was finally modified by Magellanian elements, which in some cases have to be accepted as phylogenetic old forms. Other available information on Crustacea, especially for Cirripedia, Ostracoda, Decapoda, and Isopoda support this interpretation. Therefore, it may be assumed that the Recent Antarctic crustacean fauna was established mainly about 38 m. y. ago. Practically no primitiv forms exist in this region, i. e. there are no relict species. On the contrary, we have to suggest that an important part of the fauna is represented by apomorphic species which have reached the Antarctic shelf from the deep sea. Polar emergence is a more likely hypothesis at the moment than tropical submergence. However, the final elucidation of this question can be given only after detailed phylogenetic analysis of the fauna of the adjacent deep sea basins.     

Stelar structure ofAsplenium obtusifolium and its allied species in the New World tropics,with comparison to the Asian members ofAsplenium sect.Hymenasplenium

The stelar structure ofAsplenium obtusifolium and its related species (A. repandulum, A. riparium, A. triquetrum, A. volubile, A. purpurascens, A. ortegae, A. delitescens, A. hoffmannii, andA. laetum) in the New World tropics was observed and compared to that of Asian species ofAsplenium sect.Hymenasplenium. Both of the groups were found to share peculiar stelar structures: steles with two meristeles, a broader ventral and a narrower dorsal, each providing one of the two leaf traces; leaf gaps arranged in two rows between the dorsal and ventral strands, which are connected by thin meristeles, delimiting the leaf gaps. These structures are distinct from the radial symmetrical ones general inAsplenium. Together with cytological evidence, this strongly indicates that the New and Old World groups are closely related. Thus, these Neotropical species should be included in sect.Hymenasplenium.     

Convoluted history and confusing morphology: Molecular phylogenetic analysis of dicrocoeliids reveals true systematic position of the Anenterotrematidae Yamaguti, 1958 (Platyhelminthes,Digenea)

The Dicrocoeliidae is a highly diverse family of digeneans parasitic in amniotic tetrapods. Detailed molecular phylogenetic analysis of dicrocoeliids is lacking and only a few dicrocoeliids from mammals have been included in previous studies. Sequence data were previously absent for the Anenterotrematidae that shares several morphological characteristics with dicrocoeliids. We examined phylogenetic affinities of several newly sequenced (nuclear 28S rDNA) taxa of dicrocoeliids and anenterotrematids collected from small mammals in Ecuador, Panama, Peru, USA and Vietnam. Our analyses demonstrated that the two anenterotrematid genera (Anenterotrema, Apharyngotrema) belong to the Dicrocoeliidae, placing the Anenterotrematidae into synonymy with the Dicrocoeliidae. Molecular data combined with morphological examination of type and new specimens provided evidence that Parametadelphis and Apharyngotrema are junior synonyms of Metadelphis, with all Metadelphis species lacking a digestive system. Phylogenetic analysis demonstrates that reduction of the alimentary tract in Lutztrema and its loss in Anenterotrema and Metadelphis represent at least two independent evolutionary events. Genera Brachylecithum, Brachydistomum, and Lyperosomum proved to be non-monophyletic, each likely representing more than a single genus. Furthermore, phylogenetic analysis did not support monophyly of the two largest subfamilies of the Dicrocoeliidae (Dicrocoeliinae and Leipertrematinae) with the other two subfamilies not included in this study. Therefore, we propose to abandon the current subfamily division of the Dicrocoeliidae. Analysis of host associations indicates multiple host-switching events throughout evolution of dicrocoeliids. Lastly, analysis of dicrocoeliid geographic distribution revealed that nearly all major clades included taxa from more than a single zoogeographic realm with the exception of the clade Anenterotrema?+?Metadelphis, found only in the Neotropics.     

Morphology,zoospore ultrastructure,and molecular position of taxa in the Asterophlyctis lineage (Chytridiales, Chytridiomycota)

The purpose of our research is to investigate morphology, zoospore ultrastructure, and molecular placement of six strains in the Asterophlyctis (Chytridiales) lineage. In previous molecular analyses strain JEL 186, putatively Asterophlyctis sarcoptoides, placed as basal in family Chytriomycetaceae. Recent sampling for chytrids resulted in isolation of five strains (WJD 209, MP 058, JEL 524, JEL 857, and JEL 885) molecularly related to strain JEL 186. Our morphological evaluations reveal that strains JEL 186 and WJD 209 are members of Asterophlyctis. Strain WJD 209 is considered representative of the type, A. sarcoptoides, and strain JEL 186 a new species, Asterophlyctis michiganensis. The four strains MP 058, JEL 524, JEL 857, and JEL 885 are distinct from Asterophlyctis, and we consider them as members of a new genus, Wheelerophlyctis, composed of two species, Wheelerophlyctis interior and Wheelerophlyctis interiexterior. Asterophlyctis and Wheelerophlyctis are sister taxa and we demarcate that lineage as Asterophlyctaceae. The two genera also have similar zoospore ultrastructure, which is unique among strains in Chytridiales. In consideration of their molecular position and zoospore ultrastructure, we hypothesize that Asterophlyctis and Wheelerophlyctis represent a bridge between Chytriomycetaceae and Chytridiaceae. This research expands our concepts of systematics and zoospore ultrastructural variation in Chytridiales.     

Rhinocerotidae (Mammalia,Perissodactyla) from the middle Pleistocene levels of Grotta Romanelli (Lecce,southern Italy)

The rhinoceros remains collected during the past century in the lower levels XII (= K) and XI (= I) of the famous Pleistocene locality of Grotta Romanelli (Lecce, southern Italy) are described and compared in detail for the first time. Some remains are referred to Stephanorhinus sp. and others are assigned here to the late early-middle Pleistocene European species Stephanorhinus hundsheimensis based on several morphological characters. Based on its olivine-bearing texture, the volcanoclastic ash sampled from some rhinoceros bones can be referred to the first phase of the Monte Vulture activity (around 630 ka). The results of the stable isotope analyses suggest that the climate in the lowest levels of Grotta Romanelli could have been more arid than it was at the time of the upper level IX, which is generally referred to the late Pleistocene. In addition, both recent day δ¹⁸O_ppt values and MAT are very similar to values calculated for levels X and XII, suggesting that the climate at those times may have been close to the Present one, whereas climate in level IX may have been somewhat cooler. The presence of Stephanorhinus hundsheimensis suggests a middle Pleistocene age for the lower levels of Grotta Romanelli, in agreement with the results obtained from the volcanoclastic material.