Tetrahydroisoquinoline alkaloids and 2-deoxyribonolactones from Aristolochia arcuata

2-Deoxyribonolactones and four tetrahydroisoquinoline alkaloids were isolated from the acetone extract of the leaves of Aristolochia arcuata Mast., together with pinitol, sequoyitol, glycerol, fructose, sucrose, eupomatenoid-7, salsolinol, and 6,7-dihydroxyl,1-dimethyl-1,2,3,4-tetrahydroisoquinoline. Their structures were determined on the basis of spectroscopic methods, mainly using H-1, C-13, N-15, and P-31 NMR. (C) 2003 Elsevier B.V. Ltd. All rights reserved.

ALKALOIDS FROM ARISTOLOCHIA-ARCUATA

Phytochemical studies with Aristolochia arcuata led to the isolation of KNO3, fructose, sucrose, sitosterol, calarene, its 2-oxo derivative, and three neolignans. Besides which, two new 13-oxidodibenzo[a, g]-quinolizinium alkaloids were isolated. They present only one oxygenated substituent at rings A and D.

Preferência alimentar e desenvolvimento de Cerotoma arcuata (Olivier) (Coleoptera: Chrysomelidae) em soja

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

The Adolpho Lutz collection of Tabanidae: (Diptera): I. The described genera and species, condition of the collection, and selection of lectotypes

A study of the Adolpho Lutz Collection of Tabanidae at the Instituto Oswaldo Cruz and of additional Lutz material at the Instituto Butantan in São Paulo is reported. Of the ninety-four species of Tabanidae validly described by Lutz, type material of eighty-four was recognized, either holotypes, allotypes or syntypes. Lectotypes were selected from among syntype series or remaining specimens and all type material was labelled. Of the ten species of which no type material could be found, neotypes were designated in the case of two species, Erephosis nigricans and Erephosis pseudo-aurimaculata. Types of three species, Chrysops ecuadoriensis, Dichelacera salvadorensis and Esenbeckia nigricorpus are believed to have been in Hamburg and destroyed during the last war. Types of two species, Esenbeckia biscutellata and E. dubia, and additional type material of several others are believed to have been in Montevideo. A request for information about them remains unanswered. Types of the remaining three species, Dichelacera intermedia, Dichelacera laceriascia and Esenbeckia distinguenda could not be found, and it is believed that at least the type of the last species was accidentally destroyed. Three specific of subspecific names proposed by Lutz but palaced by others in synonymy have been revalidated, Acanthocera intermedia, Erephosis brevistria and Esenbeckia fenestrata. Generic placement of two names has been changed, Esenbeckia arcuata ricardoae to Proboscoides, and Selasoma giganteum to Stibasoma. Seven specific names proposed by Lutz appear to be synonyms of earlier names, as follows: Bombylopsis juxtaleonina Lutz and Castro, 1936 = B. leonina Lutz, 1909. Bombylopsis pseudoanalis Lutz, 1909 = B. erythronotata (Bigot, 1892). Esenbeckia fuscipennis var. flavescens Lutz, 1909 = Esenbeckia fuscipennis Wied., 1828. Fidena chrysopyga Lutz and Castro, 1936 = F. atra Lutz and Castro, 1936. Laphriomyia longipalpis Lutz and Castro, 1937 = L. mirabilis Lutz, 1911. Stibasoma semiflavum Lutz, 1915 = St. bicolor Bigot, 1892. Tabanus hesperus Lutz, 1912 = Chlorotabanus (Cryptolylus) innotescens (Walker, 1854). Four Lutz names appear to antedate names proposed by others, viz.: Diachlorus angustifrons Kröber, 1930 and D. ochraceus Kröb., 1928 not Macquart, 1850 = Diachlorus fuscistigma Lutz, 1913. Psalidia fairchildi Barretto, 1950 = dicladocera conspicua Lutz and Neiva, 1914. Fidena pseudo-fulvithorax Kröb., 1931 = Erephopsis flavicrinis Lutz, 1909. Esenbeckia lemniscata Enderlein, 1925 = Esenbeckia clari Lutz, 1909. Some comments on Lutz' system of classification are given together with notes on the genotypes and included species of his genera as revaled by his collection and notes.

Caracterização de um isolado do Bean rugose mosaic virus (BRMV) de Minas Gerais e estimativa de perdas em feijoeiro em infecção simples ou em conjunto com o BCMV

Plantas de feijão-vagem do cultivar Novirex apresentando mosaico e enrolamento de vagens, sem deformação foliar evidente, foram coletadas em 2002 em Cordisburgo, MG. Estudos preliminares identificaram o vírus como um isolado do Bean rugose mosaic virus (BRMV). Este trabalho relata a caracterização do isolado, por meio de produção e avaliação de anti-soro, determinação da gama de hospedeiros, estudo da transmissão do vírus por besouros crisomelídeos e estimativa de perdas em feijoeiro como resultado de infecção isolada ou em conjunto com o Bean common mosaic virus (BCMV). O roteiro adotado para purificação possibilitou a obtenção de vírus purificado em rendimento satisfatório para a produção de anti-soro. A titulação dos anti-soros foi realizada por ELISA indireto, obtendo-se reações positivas com a diluição máxima testada (1:70.000). Das 22 espécies vegetais utilizadas na gama de hospedeiros, foram infectadas plantas de Chenopodium quinoa e alguns cultivares de feijão e soja, conforme esperado para o BRMV. O isolado de BRMV foi transmitido pelo besouro crisomelídeo Cerotoma arcuata a uma taxa de 33,3%. A infecção simples de feijão 'Ouro Negro' e de feijão-vagem 'Novirex' levou a uma redução do peso das vagens por planta de 3,4% e 84,9%, respectivamente. Infecção mista do BRMV com o BCMV levou a uma redução do peso de vagens por planta de até 70,1% para 'Novirex' e de até 90,8% para 'Ouro Negro'.

Micrasterias C. Agardh ex Ralfs (Zygnematophyceae) de duas Áreas de Proteção Ambiental da planície litorânea do norte da Bahia, Brasil

Estudo taxonômico do gênero Micrasterias C. Agardh ex Ralfs realizado em duas Áreas de Proteção Ambiental (APA Rio Capivara e APA Lagoas de Guarajuba), ambas situadas no Município de Camaçari, Estado da Bahia, nordeste do Brasil. Os materiais estudados, de origem do plâncton e do perifíton, provieram de 96 amostras coletadas no verão (dezembro de 2006 a março de 2007) e no inverno (maio a agosto de 2007), em ambientes lóticos e lênticos. Foram identificados 14 táxons, dos quais M.americana (Ehrenb.) Ralfs var. bahiensis I. B. Oliveira, C. E. M. Bicudo & C. W. N. Moura foi descrita como nova para a ciência e 10 constituem citacões pioneiras para a desmidioflórula da Bahia, quais sejam: M. alata G. C. Wall., M. arcuata Bailey var.subpinnatifida West & G. S. West f. subpinnatifida, M. borgei H. Krieg. var. borgei, M. foliacea Bailey ex Ralfs var. foliacea, M. furcata C. Agardh ex Ralfs var. furcata f. furcata, M. laticeps Nordst. var. laticeps, M. laticeps Nordst. var.acuminata H. Krieg., M. mahabuleshwarensis J. Hobson var.ampullacea (W. M. Maskell) Nordst., M. mahabuleshwarensis J. Hobson var. mahabuleshwarensis f. mahabuleshwarensis, M. pinnatifida (Kütz.) Ralfs var. pinnatifida f. pinnatifida, M. radiosa Ralfs var. elegantior (G. S. West) Croasdale, M. rotata (Grev.) Ralfs var. rotata e M. truncata (Corda) Bréb. ex Ralfs var. pusilla G. S. West. As espécies mais bem representadas na área estudada foram M. alata e M. pinnatifida presentes, respectivamente, em 50% e 45,83% das amostras analisadas. Micrasteriaslaticeps var.acuminata e M.americana var. bahiensis, foram as menos representadas, por terem sido registradas apenas em 2,08% e 1,04% respectivamente.

Molekulare Systematik der Gattung Suaeda (Chenopodiaceae) und Evolution des C4-Photosynthesesyndroms

Mit der vorliegenden Arbeit wird eine Synthese aus molekularer Phylogenie und Merkmalsentwicklung für die Unterfamilie Suaedoideae der Chenopodiaceae präsentiert. Anhand von rekonstruierten Stammbäumen aus den Sequenzunterschieden von DNA-Abschnitten zweier unabhängiger Genome (Kern, Chloroplast) werden monophyletische Gruppen herausgearbeitet und die Variabilität der molekularen Merkmale in Bezug auf die bekannten Arten diskutiert. Insgesamt wurden für alle molekularen Analysen 294 Sequenzen ausgewertet. Mit 254 Sequenzen von Arten der Unterfamilie Suaedoideae und 18 Sequenzen von Arten der Unterfamilie Salicornioideae wurde eine vergleichende molekulare Analyse mit den DNA-Regionen ITS, atpB-rbcL und psbB-psbH durchgeführt. Mit der Einbeziehung von ca. 65 bekannten Suaeda-Arten sind damit je nach Artauffassung bis zu 80% aller Arten der Gattung berücksichtigt. Mittels Fossildaten werden die wichtigsten Divergenzereignisse zeitlich fixiert. Die molekularen Stammbäume dienen weiterhin als Grundlage für die Bewertung der Arten sowie ihrer morphologischen und anatomischen Merkmale. Ein wichtiger Aspekt bildet dabei die Entwicklung der C4-Photosynthese mit den zugehörigen Blatttypen. Die folgenden vier Themenkomplexe bzw. Fragestellungen sollten bearbeitet werden (für ausführliche Darstellung vgl. Kap. 1.3): 1. Monophyletische Gruppen und ihre Beziehungen 2. Prinzipien der Evolution und Artbildung in der untersuchten Gruppe, Abgrenzung der Arten. 3. Entwicklung des C4-Photosynthesesyndroms 4. Entwicklung und Variabilität systematisch relevanter Merkmale Die Ergebnisse der auf vergleichender DNA-Sequenzierung beruhenden molekularen Analyse und die Synthese mit weiteren Daten führen als Resultat der vorliegenden Arbeit zusammenfassend zu folgenden Ergebnissen: 1.) Die drei sequenzierten DNA-Regionen ITS, atpB-rbcL und psbB-psbH zeigen im Vergleich eine sehr unterschiedliche Variabilität, ITS ist die variabelste aller Regionen. Die in den Alignments gefundenen Merkmale in Form von Punkt- und Längenmutationen zwischen den Einzelsequenzen waren zahlenmäßig ausreichend und qualitativ geeignet, um mit den drei Verfahren Maximum Parsimony, Maximum Likelihood und Bayes’scher Analyse aussagekräftige und in wesentlichen Aussagen kongruente molekulare Phylogenien zu rekonstruieren. Die Chloroplasten-Daten wurden für die Berechnungen kombiniert. 2.) Die beiden DNA-Regionen ITS und atpB-rbcL evolvieren mit sehr unterschiedlichen Geschwindigkeiten. Die mit der Glättungsmethode PL berechneten durchschnittlichen Substitutionsraten weisen für ITS eine 5,5fach höhere Substitutionsrate gegenüber atpB-rbcL nach. Die ITS-Sequenzen sind daher wesentlich diverser und für einige Sippen, bei identischen atpB-rbcL-Sequenzen, unterschiedlich. Eine direkte Homologisierung von molekularer und morphologischer Variabilität oder die molekulare Limitierung von Arten ist daher nur in einigen Fällen möglich. 3.) Die Gattungen Suaeda, Alexandra und Borszczowia bilden eine monophyletische Gruppe, die den Salicornioideae als Schwestergruppe gegenübersteht. Dies bestätigt die Ergebnisse der Phylogenie der Chenopodiaceae (Kadereit et al. 2003). Im traditionellen Verständnis ist damit die Gattung Suaeda paraphyletisch. Durch taxonomische Umkombination (Schütze et al. 2003. Kapralov et al. 2006) werden die Gattungen Alexandra und Borszczowia in Suaeda eingegliedert, womit das Monophylie-Kriterium für die Gattung wieder erfüllt ist. Die molekularen Daten unterstützen diese nomenklatorische Neubewertung. Der nachfolgend verwendete Gattungsname Suaeda bezieht sich auf die neue Fassung. 4.) Bienertia gehört nicht in die unter 2.) beschriebene monophyletische Gruppe. Die Stellung dieser Gattung ist intermediär. Im ITS-Baum bildet sie die Schwestergruppe zu den Salicornioideae, im Chloroplasten-Baum diejenige zu Suaeda. Da Bienertia aufgrund morphologischer Merkmale Suaeda ähnlicher ist als den Salicornioideae wird sie in die intern neu gegliederte Unterfamilie der Suaedoideae einbezogen, die weitgehend der in Ulbrich (1934) vertretenen Auffassung entspricht. 5.) Suaeda teilt sich in zwei sehr deutlich getrennte Gruppen, die in einer neuen Gliederung als Untergattungen Brezia und Suaeda definiert werden. Die Trennung datiert mit etwa 30 Mio. Jahren in das Oligozän. Zur Untergattung Brezia gehören alle Arten der Sektion Brezia nach bisheriger taxonomischer Auffassung, die Untergattung Suaeda vereint alle übrigen Arten und wird in weitere Sektionen untergliedert. 6.) Die Untergattung bzw. Sektion Brezia zeigt im ITS-Baum eine deutliche Dreigliederung in 3 Subclades, die allerdings von den Chloroplasten-Bäumen nicht verifiziert wird und auch durch morphologische Merkmale nicht zu rechtfertigen ist. Die Subclades der Untergattung Suaeda entsprechen in Grundzügen den bisherigen Sektionen und sind durch synapomorphe Merkmale gekennzeichnet. Für die Gattung Suaeda leiten sich nach monophyletischen Gruppen oder singulären Linien folgende Sektionen ab: Brezia, Alexandra, Borszczowia, Schanginia, Schoberia Salsina (inkl. der früheren Sektionen Limbogermen, Immersa und Macrosuaeda), Suaeda, Physophora und Glauca (neu). 7.) Hybridisierung und Polyploidisierung sind wichtige Prozesse der sympatrischen Artbildung innerhalb der Suaedoideae und waren wahrscheinlich immer mit Arealerweiterungen gekoppelt. Mehrere Linien sind durch Vervielfachung des Chromosomensatzes charakterisiert, wobei auch die recht seltene Form der Dekaploidie erreicht wird. Vieles spricht dafür, dass sowohl Auto- als auch Allopolyploidie eine Rolle spielt. Auf Autopolyplodie beruhen höchstwahrscheinlich die unterschiedlichen Chromosomenrassen von S. corniculata. Durch Inkongruenzen zwischen Chloroplasten- und ITS (Kern)-Stammbäumen konnten einige Arten mit hoher Wahrscheinlichkeit als etablierte, allopolyploide Hybridsippen identifiziert werden (Suaeda kulundensis, S. sibirica). Es ist damit erwiesen, dass die Diversifizierung durch retikulate Evolution beeinflusst wird. 8.) Die Ergebnisse der molekularen Phylogenien belegen sehr deutlich, dass sich die C4-Photosynthese innerhalb der Suaedoideae viermal unabhängig mit vier vollkommen unterschiedlichen Blatttypen entwickelt hat. Dazu gehören zwei Blatttypen mit single cell C4-photosynthesis, ein bis vor kurzem bei Landpflanzen unbekanntes Phänomen. Innerhalb der Sektionen Schoberia, Salsina und Borszczowia datiert die Entstehung in das späte Miozän, bei Bienertia entstand die C4-Photosynthese möglicherweise noch früher. 9.) Als systematisch äußerst bedeutsame Merkmale haben sich die schon von Iljin (1936a) benutzten Pistill-Formen sowie spezifische Blattmerkmale herausgestellt. Mit diesen Merkmalen können Sektionen, die auf monophyletischen Gruppen beruhen, gut definiert werden. Synapomorphe Merkmale des Pistills sind die Zahl und Ausbildung der Narben sowie die Form ihrer Insertion im Ovar. Bei den Blatttypen sind es vor allem die vier histologisch hoch differenzierten C4-Blatttypen, die als gemeinsam abgeleitetes Merkmal rezenter, teilweise aufgespaltener Linien gewertet werden. 10.) Die früher z.T. überbewerteten Merkmale des Perianths (Verwachsungen, Flügel, Anhänge und Umbildungen) können nur zur Beschreibung einzelner Sippen oder lokaler Gruppen herangezogen werden. Ebenso ist das Merkmal der Lebensformen (Therophyten, Chamaephyten) kaum zur Charakterisierung von Gruppen geeignet. Wie das Beispiel Brezia sehr deutlich zeigt, kam es allein in dieser Gruppe mehrfach zur Entwicklung ausdauernder, verholzender Sippen. Der umgekehrte Prozess fand bei der Entstehung der annuellen S. aegyptiaca und S. arcuata statt. Mit Hilfe von DNA-basierten Stammbäumen ist es in der vorliegenden Arbeit möglich geworden, die evolutionäre Geschichte der Gattung nachzuzeichnen und eine auf monophyletischen Gruppen basierende Gliederung abzuleiten. Damit wird eine Grundlage für ein verbessertes Artkonzept der Gattung Suaeda geschaffen. Für die praktische Taxonomie ist dies aber nur teilweise bedeutend. Die morphologisch nachvollziehbare Abgrenzung von Arten bleibt, gerade in den diversen Sektionen Brezia und Salsina, umstritten und kaum nachvollziehbar. Ein Großteil der Arten hat offenbar keine interspezifischen Kompatibilitätsschranken, es handelt sich daher um Morpho- oder Semispecies, möglicherweise sogar nur geographische Rassen, die allerdings mit schnell evolvierenden DNA-Regionen wie ITS differenzierbar sind. Ausgehend von den Ergebnissen der vorliegenden Arbeit verbleibt genügend Raum für weiterführende, vertiefende systematische und populationsbiologische Studien.

Repelência e deterrência alimentar de vaquinhas por óleos de nim e cinamomo aplicados em folhas de feijoeiro

This work aimed to evaluate the repellent and deterrent effect of the application of concentrations of neem and chinaberry oil on bean leaves on the leaf beetles Diabrotica speciosa (Germar) and Cerotoma arcuata (Olivier). The concentrations of neem oil tested were 0.625, 1.25, 2.50, 5.00, 10.00 and 20,00 mL, corresponding respectively to 1, 2, 4, 8, 17 and 33 ppm of azadirachtin A and the concentrations of chinaberry oil used were the same used to neem oil, corresponding, however, to 1.875, 3.75, 7.50, 15.00, 30.00 and 60.00 mg mL(-1) of chinaberry extract, respectively. For the free-choice tests, glass containers were used as arenas, whereas for the no-choice tests Petri dishes were used, where in both one insect per treatment was released in the center. Attractiveness was evaluated in predetermined time periods, in addition to the leaf consumption, at the end of the experiment. Neem oil is repellent to D. speciosa and C. arcuata, with more efficient results at the 5.00, 10.00 and 20.00 mL concentrations. All concentrations of neem oil reduce leaf consumption of both insects, except in the no-choice test with D. speciosa, in which only the 10.00 and 20.00 mL concentrations are deterrent. Chinaberry oil provides high repellent activity on both leaf beetle species, and the 10.00 and 20.00 mL concentrations stood out. The 10.00 and 20.00 mL concentrations of chinaberry oil are deterrent to D. speciosa and C. arcuata.

Mating Behavior of Diabrotica speciosa (Coleoptera: Chrysomelidae)

Diabrotica speciosa (Germar) is an economically important pest of Neotropical cultures and represents a quarantine risk for Neartic and Paleartic Regions. Despite its agricultural importance, few studies have been done on mating behavior and chemical communication, which has delayed the development of behavioral techniques for population management, such as the use of pheromone traps. In this study, we determined 1) the age at first mating; 2) diel rhythm of matings; 3) number of matings over 7 d; 4) the sequence of D. speciosa activities during premating, mating, and postmating; 5) the duration of each activity; and 6) response to male and female conspecific volatiles in Y-tube olfactometer. The first mating occurred between the third and seventh day after adult emergence and the majority of pairs mated on the fourth day after emergence. Pairs of D. speciosa showed a daily rhythm of mating with greater sexual activity between the end of the photophase and the first half of the scotophase. During the 7 d of observation, most pairs mated only once, although 30% mated two, three, or four times. In a Y-tube olfactometer, males were attracted by virgin females as well as by the volatile compounds emitted by females. Neither males nor their volatiles were attractive to either sex. Our observation provide information about mating behavior of D. speciosa, which will be useful in future research in chemical communication, such as identification of the pheromone and development of management techniques for this species using pheromone traps.

Foraminifera and microfossil occurence in Late Jurassic sediments of the North and South Atlantic

Biostratigraphical, taxonomical, and palaeocological results were obtained from Oxfordian to Tithonian foraminifers of the Northern and Southern Atlantic Ocean boreholes of the DSDP Legs 1, 11, 36, 41, 44, 50, and 79. An oversight on the cored Jurassic sections of the DSDP Legs 79 and the corresponding foraminiferal descriptions are given. The reddish brown, clayey and carbonaceous Cat Gap Formation (Oxfordian to Tithonian) of the Northern Atlantic Ocean, rich in radiolarians, yields less or more uniform, in most cases allochthonous foraminiferal faunas of Central European shelf character. No Callovian and Upper Tithonian foraminiferaI zones can be established. The zone of Pseudomarssonella durnortieri covers the Oxfordian/Kimmeridgian, the zone of Neobulimina atlantica the Kimmeridgian/Lower Tithonian interval. Characteristic foraminiferal faunas are missing since the Upper Tithonian to Valanginian for reason of a widely distributed regression which caused hiatuses observed all over the Northern Atlantic Ocean and in parts of Europe. The Upper Jurassic cannot be subdivided into single stages by foraminiferal biostratigraphy alone. The fovaminiferal zones established by Moullad (1984) covering a Callovian-Tithonian interval may be of some local importance in the Tethyan realm: It has too long-ranging foraminiferal species to be used as index marker in the word-wide DSDP boreholes. Some taxonomical confusion is caused because in former publications some foraminiferal species have got different names both in the Jurassic and Cretaceous. The foraminiferal biostratigraphy of drilled sections from DSDP boreholes is restricted by the drilling technique and for palaeo-oceanographical, biological, and geological reasons. Foraminiferal faunas from the DSDP originally described as ,,bathyal, or ,,abyssal,, have to be derived from shallower water. This contrasts the palaeo-water depths of 3000-4000 m which result from sedimentological and palaeo-geographical investigations.

Mean cover and frequencies of vascular plant species during three decades around Abisko Scientific Research Station

Plant species distributions are expected to shift and diversity is expected to decline as a result of global climate change, particularly in the Arctic where climate warming is amplified. We have recorded the changes in richness and abundance of vascular plants at Abisko, sub-Arctic Sweden, by re-sampling five studies consisting of seven datasets; one in the mountain birch forest and six at open sites. The oldest study was initiated in 1977-1979 and the latest in 1992. Total species number increased at all sites except for the birch forest site where richness decreased. We found no general pattern in how composition of vascular plants has changed over time. Three species, Calamagrostis lapponica, Carex vaginata and Salix reticulata, showed an overall increase in cover/frequency, while two Equisetum taxa decreased. Instead, we showed that the magnitude and direction of changes in species richness and composition differ among sites.

Benthic foraminifera in Lower Cretaceous sediments from various DSDP samples

From the DSDP Legs 1, 11, 13, 17, 25, 27, 32, 36, 41, 43, 44, 50, and 62 the Lower Cretaceous foraminifers have been investigated for biostratigraphical, taxonomical, and palaeoecological purposes. An overview of the cored Lower Cretaceous sections of Leg 1-80 is given. In the Northern Atlantic Ocean characteristic foraminiferal faunas are missing from the Upper Tithonian to the Valanginian due to a marked regression which caused hiatuses. In areas without black shale conditions Valanginian to Barremian medium rich to poor microfaunas with Praedorothia ouachensis (Sigal) of the Praedorothia ouachensis Zone (Valanginian-Hauterivian). The Hauterivian-Aptian interval is characterized by zones of Gavelinella barrerniana, Gaudryina dividens, and Conorotalites aptiensis. During the Albian a world-wide fauna consisting of agglutinated and calcareous foraminifers of the Pseudoclavulina gaultina Zone is established in areas lacking the wide-spread black-shale conditions. The Upper Albian and the Cenomanian are represented by the Gavelinella eenomanica Zone. Some ornamented species of the nodosariids (Citharina, Lenticulina), Gavelinella, Conorotatites, Pleurostomella, Vatvulineria, and Osangularia are of some importance for the biostratigraphy of the Berriasian-Albian interval. The Berriasian to Albian zones introduced for the Tethys and the DSDP by Moullade (1984) could only be of some local importance due to the long stratigraphical range of the foraminiferal species used. In the Indian Ocean an exact stratigraphical age cannot be assigned to the few Neocomian foraminiferal faunas of a cooler sea water (Site 261). These faunas mainly contain primitive agglutinated foraminifers, because in most cases the calcareous tests are dissolved or redeposited. In the Pacific Ocean most of the Berriasian to Aptian microfaunas are of minor biostratigraphical and palaeoecological importance for reasons of poor core recoveries, contaminations or original foraminiferal poverty (black shales). Since the Albian there are somewhat higher-diverse faunas of calcareous and agglutinated foraminifers with index species of the Pseudoclavulina gaultina Zone. As a rule, the boundary Albian/Cenomanian is set by means of planktonic foraminifers because no other foraminifer has its first appearance datum during this interval, except Gavelinella cenornanica. During the Albian very uniform, world-wide foraminiferal faunas without a marked provincialism are obvious.

Jurassic microfossils of DSDP Hole 79-547B

The first marine incursion of the incipient North Atlantic Ocean is recorded in the uppermost Triassic to Lower Jurassic sequence of DSDP Site 547 off central Morocco. A lithologic change from continental red beds below to slope breccias and hemipelagic carbonates above indicates that a carbonate ramp was probably established by Sinemurian time along the Moroccan continental margin and that subsidence in the adjacent basin was rapid in the early phases of continental rift. Foraminifers recovered from the Liassic (Sinemurian-Pliensbachian) basinal deposits are diverse and well preserved. The faunas are compositionally similar to contemporaneous neritic assemblages of Europe and the Grand Banks of Newfoundland. The Middle Jurassic in Hole 547B is characterized by regressive deposits that are poor in foraminifers. The major Late Jurassic "Atlantic" transgression is again represented by basinal deposits consisting of limestone breccias and pelagic carbonates. Foraminifers recovered from this interval are transitional between Late Jurassic assemblages reported from deep-sea deposits in the North Atlantic and typical Late Jurassic neritic assemblages of Europe. The Late Jurassic assemblages of Hole 547B are primarily dominated by nodosariids and spirillinids with moderate abundances of simple arenaceous forms. Nonreticulate epistominids occur very rarely in the Upper Jurassic of Hole 547B. It is tentatively suggested that these represent upper bathyal assemblages.

Tab. 1: Distribution of important species along a topographical transect in a siliceous boulder talus near Vårsolbukta, Bellsund

The vegetation pattern of siliceous boulder snow beds (Dicranoweision crispulae all. nov. prov.) of Svalbard was investigated by using transect studies in several places on Spitsbergen. Dicranoweisia crispula is the best diagnostic species. It is found throughout the whole snow bed, is a good differential species against Racomitrium lanuginosum communities above the snow bed, and does not occur on basic rocks. Three Andreaea spp. are also among the most important members of these communities. They are all acidophilous, but with different pH preferences. Eight weakly acidophilous species lacking both on basic and on gneissic/granitic rocks, are reported from Svalbard. Half of these are characteristic species of Dicranoweision crispulae on Svalbard.