Svensk historisk bibliografi.

Imprint varies.

Botanisches Zentralblatt. B.B.C. Beihefte.

Beginning with v. 18, 1904-05, issued in 2 pts.: Abt. A. Morphologie und Physiologie der Pflanzen (1905- Anatomie, Histologie, Morphologie und Physiologie der Pflanzen); Abt. B. Systematik, Pflanzengeographie, angewandte Botanik, etc.

Die kultur der gegenwart : ihre entwicklung und ihre ziele.

3:4:2 Zellen-und gewebelehre, morphologie unt entwicklungsgeschichte -- v. 3:4:3. Physiologie und ökologie. I. Botanischer teil, unter redaktion von G. Haberlandt. -- v. 3:4:4. Abstammungslehre. Systematik paläontologie. Biogeographie. -- v. 3:5. Anthropologie, unter leitung von G. Schwalbe und E. Fisher. 1923 -- v. 3:7:1. Naturphilosophie, unter redaktion von C. Stumpf. -- v. 4:12. Technik des kriegswesens.

[Abhandlungen über die Bildung der Eier der Vögel und Reptilen.

"Collection of reprints from Zeitschrift für wissenschaftliche zoologie und zoologischer anzeiger."

Beihefte zum botanischen Centralblatt.

Title from cover.

Systematische Phylogenie : Entwurf eines natürlichen Systems der Organismen auf Grund ihrer Stammesgeschichte /

Includes bibliographical references and indexes.

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.

Schwermineral-Untersuchungen in quartär-zeitlichen Sanden nordwestlich von Hannover

A total of 117 samples of quarternary sediments, mostly sands, from a region NW of Hannover (Lower Saxony) has been investigated with regard to their content of heavy minerals. The absolute percentage of transparent heavy minerals approximates 0.2 Vol.%. If several samples of glaciofluvial sands (Drenthe-stage) or dune sands (Late Weichsel-stage to Holocene) are taken from one outcrop they show great similarities in their heavy minerals contents. Glaciofluvial sands of the Elster-stage evidently have less Garnet, Hornblende and minerals of volcanic origin (Augite, partly also Orthopyroxenes, Oxyhornblende and Olivine) than those of the Drenthe-stage, Weichsel-stage, and the Holocene. All these groups hold nearly the same average assemblages of heavy mineral, thus indicating that within the Drenthe-stage or later material from north and from south has been mixed and/or reworked. In the area investigated the proportions of heavy minerals do not help to identify either the stratigraphic position or the way of deposition of different sandy sediments younger than the Elster-stage. The distributional pattern of several heavy minerals point out that Kyanite, Hornblende and Epidote have been transported predominantly from the north, whereas Garnet and Staurolite have sources both in the north and the south. Tourmaline, Apatite and the minerals of volcanic origin mainly must be derived from the south. All results obtained in the region examined should not be transferred to other zones of the lowlands of Northern Germany automatically.

Ein Profil von den Ornaten-Schichten (Callovium-Dogger) bis zum unteren Korallenoolith (Oxfordium-Malm) im Grubenfeld Konrad , Salzgitter-Bleckenstedt (Ostniedersachsen)

Im Grubenfeld "Konrad" der Salzgitter-Erzbergbau AG bei Salzgitter-Bleckenstedt wurde ein 62 m mächtiges, von den Ornaten-Schichten (Mittel-Callovium, coronaten-Zone) bis an die Basis des Mittleren Korallenoolith (Mittel-Oxfordium, plicatilis-Zone oder Ober-Oxfordium, cautisnigrae-Zone) reichendes Profil aufgenommen und untersucht. Die Mächtigkeit der Heersumer Schichten beträgt nur 1,5 m, die des Unteren Korallenoolith ca. 60 m. Im Gegensatz zum nördlichen Teil des Gifhorner Troges (SEITZ 1950) ist die Mächtigkeit der Heersumer Schichten im südlichen Teil also erheblich geringer. Der Untere Korallenoolith ist in beiden Vorkommen etwa gleichmächtig entwickelt. Die Schichtlücke zwischen Mittel-Callovium und Unter-Oxfor- dium, die im untersuchten Profil nachgewiesen werden konnte, tritt auch am nördlichen Harzrand in der Grube "Hansa" (DENG- LER 1954) und im Wiehengebirge (LANGE 1971) auf. Offensichtlich ist sie jedoch nur lokal entwickelt, denn im Hildesheimer Jurazug (VINKEN 1974, 1975), im nördlichen Teil des Gifhorner Troges (SEITZ 1950) und am nördlichen Harzrand in unmittelbarer Nähe der Grube "Hansa" (s.o.) liegen lückenlose Profile vor. Daß diese Schichtlücken auch im Südteil des Gifhorner Troges auftreten, spricht für ein späteres Einsetzen der Trogtendenz in diesem Gebiet. Die untersuchten Schichten stimmen in ihren wesentlichen faziellen und petrographischen Merkmalen mit benachbarten Vorkommen überein. Die Zyklen im Unteren Korallenoolith werden als Ergebnis sich ablösender Transgressions- und Regressionsphasen gedeutet.

First comprehensive multi-tissue transcriptome of Cherax quadricarinatus (Decapoda: Parastacidae) reveals unexpected diversity of endogenous cellulase

The Australian freshwater crayfish species, Cherax quadricarinatus Von Martens, 1868, is an important commercial and invasive species that is also being increasingly used as a model organism to address important and interesting questions in crustacean biology. Through deep sequencing of the transcriptome of C. quadricarinatus from the hepatopancreas and four other tissues, we examine the evolution of endogenously transcribed cellulase genes and provide new insights into controversial issues regarding the nutritional biology of crayfishes. A cluster assembly approach yielded one of the highest quality transcriptome assemblies for a decapod crustacean to date. A total of 206,341,872 reads with an average read length of 80 bp were generated from sequencing the transcriptomes from the heart, kidney, hepatopancreas, nerve, and testis tissues. The assembled transcriptome contains a total of 44,525 transcripts. A total of 65 transcripts coding for carbohydrate-active enzymes (CAZy) were identified based on hidden Markov model (HMM), and a majority of them display high relative transcript abundance in the hepatopancreas tissue, supporting their role in nutrient digestion. Comprehensive phylogenetic analyses of proteins belonging to two main glycosyl hydrolase families (GH9 and GH5) suggest shared ancestry of C. quadricarinatus cellulases with other characterized crustacean cellulases. Our study significantly expands the number of known crustacean-derived CAZy-coding transcripts. More importantly, the surprising level of evolutionary diversification of these proteins in C. quadricarinatus suggests that these enzymes may have been of critical importance in the adaptation of freshwater crayfishes to new plant-based food sources as part of their successful invasion of freshwater systems from marine ancestors.