Kern-Schale-Katalysatorsysteme in der Polyolefinpolymerisation

Das Ziel der vorliegenden Arbeit war die Synthese eines Katalysatorpartikels, der in der Lage ist, in nur einem Polymerisationsschritt einen Kern-Schale-artigen Produktpartikel herzustellen, bei dem zwei verschiedene Polyolefine jeweils ortsaufgelöst in der Schale bzw. im Kern vorhanden sein sollten. Dabei wurden zwei Grundbedingungen erfüllt: Optimale Trennung der verschiedenen Katalysatordomänen in Kern und Schale; diese Trennung durfte auch bei den in industriellen Polymerisationen herrschenden Reaktionsbedingungen (Druck, Scherkräfte, Temperatur, Lösungsmittel) nicht verloren gehen. Beibehaltung der Aktivität und Spezifität der einzelnen Katalysatoren; dabei muß besonderes Augenmerk auf den Kern gelegt werden, der ggf. durch die aufzutragende Schale nicht ausreichend mit Monomer versorgt wird oder während dem Aufbringen der Schale desaktiviert werden könnte. Die entwickelte Trägerungsroute besticht durch das simple Trägerungsverfahren des Schalenmaterials und des Schalenkatalysators, bedingt durch die Affinität der funktionalisierten Schalenpartikel mit dem Kernkatalysatorsystem. Die entwickelte Trägerungsroute kann industriell mit allen gängigen (Post)Metallocenen sowie (als Kernpartikel) Ziegler-Natta-Systemen anwendbar sein und ist hierdurch sehr flexibel.

Identificazione di markers morfologici e sierologici di vulnerabilità della placca carotidea

Introduzione: L’indicazione alla rivascolarizzazione carotidea è comunemente posta in base alla percentuale di stenosi, alla presenza di sintomi neurologici ed alle condizioni cliniche del paziente. Una placca ad elevato potenziale embolico viene definita “vulnerabile”; la sua caratterizzazione, tuttavia, non è universalmente accettata ai fini della rivascolarizzazione. Lo scopo dello studio è indagare il ruolo del mezzo di contrasto ecografico (CEUS) nell’identificazione della placca carotidea vulnerabile. Materiali e Metodi: I pazienti sottoposti a endoarterectomia carotidea, sono stati valutati mediante TC cerebrale preoperatoria e CEUS. Le microbolle di contrasto rilevate nella placca, indicative di neovascolarizzazione, sono state quantificate in dB-E ed istologicamente valutate per cinque caratteristiche: (densità dei microvasi, spessore del cappuccio fibroso, estensione delle calcificazioni, infiltrato infiammatorio e core lipidico) il valore da 1 a 5, ottenuto in cieco, indica in grado di vulnerabilità della placca. L'ANOVA test, il test di Fisher e t Student sono stati usati per correlare le caratteristiche dei pazienti ed istologiche col valore di dB-E. Risultati: Di 22 pazienti (range 2-7.8, media 4.85 ±1.9 SD) vi era un numero più alto di sintomatici (7.40 ± 0.5) rispetto agli asintomatici (3.5 ± 1.4) (p = 0.002). Un più alto valore di dB-E si associava con la presenza di un sottile cappuccino fibroso (<200 µm, 5.96±1.5 vs. 3 ± 1,p = 0.01) ed un maggiore infiltrato infiammatorio (3.2 ± 0.9 vs. 6.4 ± 1.2, p = 0.03). Placche con vulnerabilità 5 si associavano ad un valore più alto di dB-E rispetto alle placche con vulnerabilità 1 (7.6 ± 0.2 vs. 2.5 ± 0.6, rispettivamente, p=0.001). Preoperatoriamente, le lesioni emboliche ipsilaterali alla TC, correlavano con un più alto valore di dB-E (5.96±1.5 vs. 3.0±1.0, p=0.01). Conclusioni: Il valore di dB-E alla CEUS indica l’estensione della neovascolarizzazione della placca carotidea e può essere utilizzato come marker di vulnerabilità della placca.

Die funktionelle Bedeutung von MSP und Lactadherin im Rahmen der Atherosklerose

Im Rahmen dieser Arbeit wurde der Einfluss zweier möglicher Biomarker auf die Atherosklerose untersucht.rnMilk fat globule-EGF factor 8 (MFG-E8, Lactadherin) ist ein Glycoprotein, das vornehmlich von Makrophagen, glatten Muskelzellen und Endothelzellen sezerniert wird. MFG-E8-/--Mäuse zeigen vermehrt apoptotische Zellen in der atherosklerotischen Plaque, verstärkte Inflammationszeichen und vergrößerte Läsionen. In situ-Hybridisierung und Immunfluoreszenz zeigen eine starke Lactadherin-Expression in den Schaumzellen atherosklerotischer Plaques von Apo E-/-, Apo E-/-/GPx 1-/-und LDLR-/- Mäusen, vor allem in der Nähe des Lipid Core. Dort kolokalisiert Lactadherin mit dem Makrophagenmarker CD 68 und dem Chemokin Fraktalkin, das die MFG-E8 Sekretion stimuliert und so die Phagocytose forciert. Untersuchungen mittels RTD-PCR ergaben, dass Peritonealmakrophagen der Genotypen Apo E-/-, Apo E-/-/GPx 1-/- und GPx 1-/-, deren Gemeinsamkeit eine höhere Empfindlichkeit gegenüberrnoxidativem Stress ist, mehr Lactadherin exprimieren als andere Genotypen (B6, LDLR-/-). Die Inkubation muriner oder humaner Makrophagen mit oxLDL und eLDL hat keinen Einfluss auf die Expression der MFG-E8 mRNA. Der Kontakt mit apoptotischer Zellen hingegen erhöht die Expression signifikant. Lactadherin ist entscheidend für die effektive Phagozytose apoptotischer Zellen in der atherosklerotischen Läsion. Seine Expression wird vermutlich durch die Apoptose in der Nähe liegender Zellen und das verstärkte Vorkommen von ROS reguliert. Macrophage stimulating protein (MSP) übt Einfluss auf Migration, Proliferation und Phagocytose von Makrophagen aus. Seine Beteiligung an inflammatorischen Vorgängen und der Karzinogenese ist intensiv untersucht worden, nicht jedoch der Einfluss auf die Atherosklerose. Es ist bekannt, dass der SNP rs3197999 mit chronisch entzündlichen Darmerkrankungen (CED) assoziiert ist. Zudem geht er vermutlich mit einem erniedrigten Atheroskleroserisiko einher. Der Polymorphismus c2078t hat den Aminosäureaustausch R689C zur Folge. Rekombinant erzeugtes, mutantes und wildtypisches MSP induziert Migration und Proliferation bei THP-1-Makrophagen. MSPmut vermittelt dies jedoch wesentliche effektiver als MSPwt. Apoptose hingegen wird durch keine der Formen induziert. R689C führt zu einem “gain of function” des MSP-Proteins in Bezug auf die Proliferations- und Migrationsfähigkeit von Makrophagen und verändert vermutlich deren Cytokinfreisetzung. Dies führt möglicherweise zu einer erhöhten Phagocytoseeffizienz in der atherosklerotischen Läsion (erniedrigtes Atherosklerose-Risiko), und zu einer aberranten immunologischen Reaktion im Rahmen der CED (erhöhtes CED-Risiko).

Saccharide based nanocapsules - From monomer building blocks to improved capsules properties

In dieser Arbeit wurde der vielfältige Nutzen von Kohlenhydraten in Nanokapsel Systemen untersucht. Drei verschiedene Nanokapsel-Typen wurden durch Reaktion an der Grenzfläche von inversen Miniemulsionen hergestellt. Es wurde gezeigt, dass die Kohlenhydrate nach Modifizierung als Monomer an der Kapselbildung teilnehmen können, oder zur Erhöhung der Sensitivität eines verkapselten Kontrastmittels beitragen können. Im Folgenden werden die Ergebnisse der einzelnen Projekte zusammengefasst. Eine neuartige Grenzflächen-Synthese zur Herstellung von Nanokapseln wurde entwickelt und untersucht. Bei der Reaktion handelt es sich um eine Ruthenium katalysierte Olefin-Kreuzmetathese, welche für die Reaktion an der Grenzfläche angepasst wurde. Als wasserlösliches Macromonomer wurde Dextranacrylat synthetisiert. Der Reaktionspartner war ein öl-löslichen Phosphoester (Phenyldi(undec-10-en-1-yl)phosphat). Anhand von NMR-Spektren wurde gezeigt, dass die Kapselbildung auf Olefin Kreuzmetathese beruht. Im Vergleich zu konventionellen Estern haben Phosphorester eine weitere Möglichkeit zur chemischen Funktionalisierung. Dies wurde exemplarisch durch die Verwendung von fluoreszenzmarkierten Phosphoestern gezeigt. Die Markierung wurde verwendet, um die pH-induzierte Abbaubarkeit der Nanokapseln mittels Fluoreszenz-Korrelations-Spektroskopie zu beobachten. Ziel des zweiten Projekts war es, Nanostrukturen zu entwickeln, um Infektionen mit Antibiotika-resistenten Bakterien lokal zu behandeln. Dazu wurden mit Dextranmethacrylat vernetzte Poly(acrylamid) basierte Nanogele synthetisiert und Zinknitrat zugesetzt. Die Synthese der Nanogele wurde erweitert, um durch Vernetzung freier Alkoholgruppen mit Toluoldiisocyanat eine Kapselschale zu erhalten. Die Schalenbildung spiegelte sich in einer geringeren Quellbarkeit der Gel- Schale-Hybride wieder. Die erhaltenen Gel-Schale-Hybride waren in der Lage das Wachstum von zwei Methicillin-resistenten Bakterienstämmen (S. aureus) zu unterdrücken und verzögern. Die synthetisierten Hybridstrukturen könnten in der Beschichtung von Wundauflagen Verwendung finden, um bakterielle Infektionen lokal und direkt nach Ausbruch zu behandeln. Ziel des dritten Projektes war es, die wichtigen Parameter in der Herstellung von Nanokapseln mit hoher Kontrastmittel Sensitivität zu identifizieren. Relaxivität/Signalsensitivität des Kontrastmittels ist von großer Bedeutung für die Bildgebung mittels MRI, dies kann durch die Begrenzung der Mobilität des Kontrastmittels erreicht werden. Aufgrund seiner hohen Komplexstabilität und seiner klinischen Bedeutung wurde das Kontrastmittel Gadobutrol für die Verkapselung verwendet. Das Kontrastmittel wurde in Polyharnstoff-Kapseln eingeschlossen, die durch einen inversen Miniemulsion-Prozess hergestellt wurden. Um die Viskosität im Inneren der Nanokapsel zu erhöhen, wurden zusätzlich Saccharose, Dextran und Polyacrylsäure verkapselt. In Gegenwart von Saccharose konnte die Relaxivität verdoppelt werden. Dies gründet sich vermutlich auf einem Second-sphere Effekt der Saccharose, einer auf Wasserstoffbrückenbindungen beruhende Interaktion von Kontrastmittel und Saccharose.

Engineering the synthesis of lantibiotics in e. Coli by combining the cynnamicin and nisin modification systems.

I lantibiotici sono molecole peptidiche prodotte da un gran numero di batteri Gram-positivi, posseggono attività antibatterica contro un ampio spettro di germi, e rappresentano una potenziale soluzione alla crescente problematica dei patogeni multi-resistenti. La loro attività consiste nel legame alla membrana del bersaglio, che viene quindi destabilizzata mediante l’induzione di pori che determinano la morte del patogeno. Tipicamente i lantibiotici sono formati da un “leader-peptide” e da un “core-peptide”. Il primo è necessario per il riconoscimento della molecola da parte di enzimi che effettuano modifiche post-traduzionali del secondo - che sarà la regione con attività battericida una volta scissa dal “leader-peptide”. Le modifiche post-traduzionali anticipate determinano il contenuto di amminoacidi lantionina (Lan) e metil-lantionina (MeLan), caratterizzati dalla presenza di ponti-tioetere che conferiscono maggior resistenza contro le proteasi, e permettono di aggirare la principale limitazione all’uso dei peptidi in ambito terapeutico. La nisina è il lantibiotico più studiato e caratterizzato, prodotto dal batterio L. lactis che è stato utilizzato per oltre venti anni nell’industria alimentare. La nisina è un peptide lungo 34 amminoacidi, che contiene anelli di lantionina e metil-lantionina, introdotti dall’azione degli enzimi nisB e nisC, mentre il taglio del “leader-peptide” è svolto dall’enzima nisP. Questo elaborato affronta l’ingegnerizzazione della sintesi e della modifica di lantibiotici nel batterio E.coli. In particolare si affronta l’implementazione dell’espressione eterologa in E.coli del lantibiotico cinnamicina, prodotto in natura dal batterio Streptomyces cinnamoneus. Questo particolare lantibiotico, lungo diciannove amminoacidi dopo il taglio del leader, subisce modifiche da parte dell’enzima CinM, responsabile dell’introduzione degli aminoacidi Lan e MeLan, dell’enzima CinX responsabile dell’idrossilazione dell’acido aspartico (Asp), e infine dell’enzima cinorf7 deputato all’introduzione del ponte di lisinoalanina (Lal). Una volta confermata l’attività della cinnamicina e di conseguenza quella dell’enzima CinM, si è deciso di tentare la modifica della nisina da parte di CinM. A tal proposito è stato necessario progettare un gene sintetico che codifica nisina con un leader chimerico, formato cioè dalla fusione del leader della cinnamicina e del leader della nisina. Il prodotto finale, dopo il taglio del leader da parte di nisP, è una nisina completamente modificata. Questo risultato ne permette però la modifica utilizzando un solo enzima invece di due, riducendo il carico metabolico sul batterio che la produce, e inoltre apre la strada all’utilizzo di CinM per la modifica di altri lantibiotici seguendo lo stesso approccio, nonché all’introduzione del ponte di lisinoalanina, in quanto l’enzima cinorf7 necessita della presenza di CinM per svolgere la sua funzione.

Facies distribution in CRP sediment cores from the Ross Sea, Antarctica

Clasts from the Cape Roberts Project cores CRP-2/2A and CRP-3 provide indications of glacially influenced depositional environments in Oligocene and Miocene strata in the western Victoria Land Basin, Antarctica. CRP-2/2A is interpreted to represent strongly glacially influenced, unconformity bound depositional sequences produced by repeated advance and retreat of floating and grounded ice across the shelf. A similar interpretation is extended to the upper 330 meters of the CRP-3 core, but the lower part of the core records shallow marine deposition with significantly less glacial influence. Clast shape analysis from selected coarse-grained facies throughout the cored interval indicates that most clasts are glacially sourced, with little distinction between diamictite and conglomeratic facies. Three dimensional clast fabric analysis from units immediately above sequence boundaries generally display weak or random fabrics and do not suggest that grounded ice actually reached the drillsite at these intervals. Striated and outsized clasts present in fine-grained lithofacies throughout the cores provide further evidence of sub-glacially transported sediment and iceberg rafting. The distribution of these striated and out-sized clasts indicate that a significant glacial influence persisted through most of the time represented by the cores with glaciers actively calving at sea-level introducing ice-berg rafted glacial debris even in the earliest Oligocene.

Grain size analysis on CRP sediment cores from the Ross Sea, Antarctica

The upper 1200 m of pre-Pliocene sediment recovered by Cape Roberts Project (CRP) drilling off the Victoria Land coast of Antarctica between 1997-1999 has been subdivided into 54 unconformity-bound stratigraphic sequences, spanning the period c. 32 to 17 Ma. The sequences are recognised on the basis of the cyclical vertical stacking of their constituent lithofacies, which are enclosed by erosion surfaces produced during the grounding of the advancing ice margin onto the sea floor. Each sequence represents deposition in a range of offshore shelf to coastal glacimarine sedimentary environments during oscillations in the ice margin across the Western Ross Sea shelf, and coeval fluctuations in water depth. This paper applies spectral analysis techniques to depth- and time-series of sediment grain size (500 samples) for intervals of the core with adequate chronological data. Time series analysis of 0.5-l.0m-spaced grainsize data spanning sequences 9-11 (CRP-2/2A) and sequences 1-7 (CRP-3) suggests that the length of individual sequences correspond to Milankovitch frequencies, probably 41 k.y., but possibly as low as 100 k.y. Higher frequency periodic components at 23 k.y. (orbital precession) and 15-10 k.y. (sub-orbital) are recognised at the intrasequence-scale, and may represent climatic cycles akin to the ice rafting episodes described in the North Atlantic Ocean during the Quaternary. The cyclicity recorded by glacimarine sequences in CRP core provides direct evidence from the periphery of Antarctica for orbital oscillations in the size of the Oligocene-Early Miocene East Antarctic Ice Sheet.

Geochemistry of minerals in CRP sediment cores from the Ross Sea, Antarctica

Sixty-four volcanic chists, sandstones and tephras between 5.95 and 618.19 meters below sea floor (mbsf) in the Cape Roberts Project cores 2 and 2A cores (CRP-2/2A) were examined for Cenozoic and Mesozoic volcanic components, using optical and Scanning Electron Microscopy. Minerals and glass shards in a selection of samples were analysed by electron microprobe fined with an EDAX detector. Laser-Ablation ICP-Mass-Spectrometry (ICP-MS) was used to determine rare earth elements and 14 additional trace elements in glass shards, pyroxenes and feldspars in order to pin-point the onset of McMurdo Volcanic Group (MVG) activity in the stratigraphic column. Pumices in tephra layers of peralkaline phonolite composition in Unit 7.2 -between 108 and 114 mbsf - were also analysed for trace elements by ICP-MS. This tephra unit is not reworked and its isotopic age (21.44 ± 0.05 Ma) is the age of deposition. The height of the eruptive column responsible for the deposition of the tephra was probably less than 8 km; the source was local, probably within 30 km from the drill site. Phonolite of unit 7.2 of CRP-2/2A has no direct petrogenetic relation with the peralkaline trachyte in the tephra-enriched layer of CRP-1 at 116.55 mbsf. Volcanic clasts and sand grains (glass shards, aegirine-augite, anorthoclase) related to Cenozoic activity of MVG were observed only starting from Unit 9.8, where they are dated at 24.22 ± 0.06 Ma at c. 280 mbsf. In this unit the lowest- occurring basaltic glass shard is found at 297.54 mbsf. Sampled McMurdo volcanics are generally vesicular and vary in composition from alkali basalt to trachyte and peralkaline phonolite. By contrast, below 320 mbsf, aphyric or slightly-porphyritic volcanic clasts become more abundant but they are all non-vesiculated, pigeconite and ilmenite-bearing basalts and dolerite of tholeiitic affinity. These rocks are considered to be related to lava flows and associated intrusions of Jurassic age (Kirkpatrick basalts and Ferrar dolerite). As in CRP-1, McMurdo volcanics appear to derive from a variety of lithologics. Besides glaciers, a dominant role of wind transportation from exposed volcanic rocks may be inferred from the contemporary occurrence of glass shards of different compositions at depths above 297.54 mbsf. These data confirm that the onset of magmatic activity in southern Victoria Land is considerably delayed (by about 24 Ma) with respect to northern Victoria Land.

Grain size analysis of sediment coring site CRP-2 from the Ross Sea, Antarctica

The purpose of this note is to present results of grain size analyses from 118 samples of the CRP-2/2A core using sieve and Sedigraph techniques. The samples were selected to represent the range of facies encountered, and tend to become more widely spaced with depth. Fifteen came from the upper 27 m of Quaternary and Pliocene sediments, 62 from the early Miocene-late Oligocene strata (27 to 307 mbsf), and 41 from the early Oligocene strata beneath (307 to 624 mbsf). The results are intended to provide reference data for lithological descriptions in the core logs (Cape Roberts Science Team, 1999), and to help with facies interpretation. The analytical technique used for determining size frequency of the sand fraction in our samples (sieving) is simple, physical and widely practised for over a century. Thus it provides a useful reference point for analyses produced by other faster and more sophisticated techniques, such as the Malvern laser particle size analysis system (Woolfe et al., 2000), and estimates derived from measurements taken with down-hole logging tools (Bücker, pers. com., 1999).

Geochemistry on smectites in sediment cores CRP-1 and CRP-2 from the Ross Sea, Antarctica

TEM (transmission electron microscopy) observations and microanalyses on smectite microparticles in the sediments of the CRP-2A core were carried out to determine their origin (authigenic or detrital) and the source rocks. Smectites are dioctahedral and are Fe-rich members of the nontronite-beidellite series. They generally display both flaky and hairy shapes, but no large compositional difference between the two forms was observed. Flaky smectites are detrital while hairy smectites probably formed in situ through the reorganisation of previous flaky particles. The source rocks for smectites are probably represented by the McMurdo Volcanic Group to the south, but also by the Ferrar Dolerites and Kirkpatrick Basalts in the Transantarctic Mountains. CRP-2A smectites are Fe and Mg richer than those of the coeval or not coeval levels of the CIROS-I, DSDP 270 and 274 cores. The average compositions of smectite in CRP-1 and CRP-2A cores show a downcore trend toward more alluminiferous terms, which might reflect the increase of the chemical weathering processes on the continent.

Stable isotope ratios measured on molluscan from the CRP sediment cores in the Ross Sea, Antarctica

Stable isotope analyses of marine bivalve growth increment samples have been used to estimate early Oligocene (29.4 - 31.2) Ma and early Miocene (24.0 Ma) seafloor palaeotemperature from the southwestern continental margin of the Ross Sea. Measured d18O values average +2.5 ? in the early Miocene and range between +1.26 to +3.24 ? in the early Oligocene. The results show that palaeoceanographic conditions in McMurdo Sound during the mid-Cenozoic were significantly different from those of today. The minimum estimated spring through late summer seasonal temperature range was 3°C during the early Miocene and between 1 and 5°C during the early Oligocene. This compares to the equivalent modern day range of <0.5°C within the sound. Absolute seawater temperatures at <100 m depth were of the order of 5 to 7°C during both time slices, compared to modern day values of -1.4 to - 1.9°C in the same area. The results are in broad agreement with early Oligocene Mg/Ca temperature estimates from deep Atlantic foraminifera as well as estimates from local terrestrial palynology and palaeobotany.

Preliminary results and documentation of sediment cores CRP2 and CRP-2A from the Ross Sea off Cape Roberts, Antarctica

The site for CRP-2, 14 km east of Cape Roberts (77.006°S; 163.719°E), was selected to overlap the early Miocene strata cored in nearby CRP-1, and to sample deeper into the east-dipping strata near the western margin ofe he Victoria Land Basin to investigate Palaeogene climatic and tectonic history. CRP-2 was cored from 5 to 57 mbsf (metres below the sea floor) (core recovery 91 %), with a deviation resulting in CRP-2A being cored at the same site. CRP-2A reached down to 624mbsf (recovery 95%), and to strata with an age of c. 33-35 Ma. Drilling took place from 16 October to 25 November 1998, on 2.0-2.2 m of sea ice and through 178 m of water. Core fractures and other physical properties, such as sonic velocity, density and magnetic susceptibility, were measured throughout the core. Down-hole logs for these and other properties were run from 63 to 167 mbsf and subsequently from 200 to 623 mbsf, although density and velocity data could be obtained only to 440 mbsf because of hole collapse. Sonic velocity averages c. 2.0 km S-1 for the upper part of the hole, but there is an sharp increase to c. 3.0 km s-1 and also a slight angular unconformity, at 306 mbsf, corresponding most likely to the early/late Oligocene boundary (c. 28-30 Ma). Velocity then increases irregularly to around 3.6 km s-1 at the bottom of the hole, which is estimated to lie 120 m above the V4/V5 boundary. The higher velocities below 306 mbsf probably reflect more extensive carbonate and common pyrite cementation, in patches, nodules, bedding-parallel masses and as vein infills. Dip of the strata also increases down-hole from 3° in the upper 300 in to over 10° at the bottom. Temperature gradient is 21° k-1. Over 2 000 fractures were logged through the hole. Borehole televiewer imagery was obtained for the interval from 200 to 440 mbsf to orient the fractures for stress field analysis. Lithostratigraphical descriptions on a scale of 1:20 are presented for the full length of the core, along with core box images, as a 200 page supplement to this issue. The hole initially passed through a layer of muddy gravel to 5.5 mbsf (Lithological Sub-Unit or LSU 1.1), and then into a Quaternary diatom-bearing clast-rich diamicton to 21 mbsf (LSU 2. l), with an interval of alternating compact diamicton and loose sand, and containing a rich Pliocene foraminiferal fauna, to 27 mbsf (LSU 2.2). The unit beneath this (LSU 3.1) has similar physical properties (sonic velocity, porosity, magnetic susceptibility) and includes diamictites of similar character to those of LSU 2.1 and 2.2, but an early Miocene (c. 19 Ma) diatom assemblage at 28 mbsf (top of LSU 3.1) shows that this sub-unit is part of the older section. The strata beneath 27 mbsf, primary target for the project, extend from early Miocene to perhaps latest Eocene age, and are largely cyclic glacimarine nearshore to offshore sediments. They are described as 41 lithological sub-units and interpreted in terms of 12 recurrent lithofacies. These are 1) mudstone, 2) inter-stratified mudstone and sandstone, 3) muddy very fine to coarse sandstone, 4) well-sorted stratified fine sandstone, 5) moderately to well-sorted, medium-grained sandstone, 6) stratified diamictite, 7) massive diamictite, 8) rhythmically inter-stratified sandstone and mudstone, 9) clast-supported conglomerate, 10) matrix-supported conglomerate, 11) mudstone breccia and 12) volcaniclastic sediment. Sequence stratigraphical analysis has identified 22 unconformity-bounded depositional sequences in pre- Pliocene strata. They typically comprise a four-part architecture involving, in ascending order, 1) a sharp-based coarse-grained unit (Facies 6,7,9 or 10), 2) a fining-upward succession of sandstones (Facies 3 and 4), 3) a mudstone interval (Facies l), in some cases coarsening upward to muddy sandstones (Facies 3), and 4) a sharp-based sandstone dominated succession (mainly Facies 4). The cyclicity recorded by the strata is interpreted in terms of a glacier ice margin retreating and advancing from land to the west, and of rises and falls in sea level. Analysis of sequence periodicity awaits afirmer chronology. However, apreliminary spectral analysis of magnetic susceptibility for a deepwater mudstone within one of the sequences (from 339 to 347 mbsf) reveals ratios between hierarchical levels that are similar to those of the three Milankovitch orbital forcing periodicities. The strata contain a wide range of fossils, the most abundant being marine diatoms. These commonly form up to 5% of the sediment, though in places the core is barren (notably between 300 and 412 mbsf). Fifty samples out of 250 reviewed were studied in detail. The assemblages define ten biostratigraphical zones, some of them based on local or as yet undescribed forms. The assemblages are neritic, and largely planktonic, suggesting that the sea floor was mostly below the photic zone throughout deposition of the corcd sequence. Calcareous nannofossils, representing incursions of ocean surface waters, are much less common (72 out of 183 samples examined) and restricted to mudstone intervals a few tens of metres thick, but are important for dating. Foraminifera are also sparse (73 out of 135 samples) and represented only by calcareous benthic species. Changing assemblages indicate a shift from inshore environments in the early Oligocenc to outer shelf in the late Oligocenc, returning to inshore in the early Miocene. Marine palynomorplis yielded large numbers of well-preserved forms from most of the 116 samples examined. The new in situ assemblagc found last year in CRP-1 is extended down into the late Oligocene and a further new assemblage is found in the early Oligoccnc. Many taxa are new, and cannot us yet contribute to an improved understanding of chronology or ecology. Marine invertebrate macrofossils, mostly molluscs and serpulid tubes, are scattered throughout the core. Preservation is good in mudstones but poor in other lithologies. Climate on land is reflected in the content of terrestrial palynomorphs, which are extremely scarce down to c. 300 mbsf. Some forms are reworked, and others represent a low growing sparse tundra with at least one species of Nothofagus. Beneath this level, a significantly greater diversity and abundance suggests a milder climate and a low diversity woody vegetation in the early Oligocene, but still far short of the richness found in known Eocene strata of the region. Sedimentary facies in the oldest strata also suggest a milder climate in the oldest strata cored, with indications of substantial glacial melt-water discharges, but are typical of a coldcr climate in late Oligocene and early Miocene times. Clast analyses from diamictites reveal weak to random fabrics, suggesting either lack of ice-contact deposition or post-depositional modification, but periods when ice grounded at the drill site are inferred from thin zones of in-situ brecciated rock and soft-sediment folding. These are more common above c. 300 mbsf, perhaps reflecting more extensive glacial advances during deposition of those strata. Erosion of the adjacent Transantarctic Mountains through Jurassic basalt and dolerite-intruded Beacon strata into basement rocks beneath is recorded by petrographical studies of clast and sand grain assemblages. Core below 310 mbsf contains a dominance of fine-grained Jurassic dolerite and basalt fragments along with Beacon-derived coal debris and rounded quartz grains, whereas the strata above this level have a much higher proportion of basement derived granitoids, implying that the large areas of the adjacent mountains had been eroded to basement by the end of the early Oligocene. There is little indication of rift-related volcanism below 310 mbsf. Above this, however, basaltic and trachytic tephras are common, especially from 280 to 200 mbsf, from 150 to 46 mbsf, and in Pliocene LSU 2.2 from 21 to 27 mbsf. The largest volcanic eruptions generated layers of coarse (up to 1 cm) trachytic pumice lapilli between 97 and 114 mbsf. The thickest of these (1.2 m at 112 mbsf) may have produced an eruptive column extending tens of km into the stratosphere. A source within a few tens of km of the drill site is considered most likely. Present age estimates for the pre-Pliocene sequence are based mainly on biostratigraphy (using mainly marine diatoms and to a lesser extent calcareous nannofossils), with the age of the tephra from 112 to 114 mbsf (21.44k0.05 Ma from 84 crystals by Ar-Ar) as a key reference point. Although there are varied and well-preserved microfossil assemblages through most of the sequence (notably of diatoms and marine palynomorphs), they comprise largely taxa either known only locally or as yet undescribed. In addition, sequence stratigraphical analysis and features in the core itself indicate numerous disconformities. The present estimate from diatom assemblages is that the interval from 27 to 130 mbsf is early Miocene in age (c. 19 to 23.5 Ma), consistent with the Ar-Ar age from 112 to 114 mbsf. Diatom assemblages also indicate that the late Oligocene epoch extends from c. 130 to 307 mbsf, which is supported by late Oligocene nannofossils from 130 to 185 mbsf. Strata from 307 to 412 mbsf have no age-diagnostic assemblages, but below this early Oligocene diatoms and nannofossils have been recovered. A nannoflora at the bottom of the hole is consistent with an earliest Oligocene or latest Eocene age. Magnetostratigraphical studies based on about 1000 samples, 700 of which have so far undergone demagnetisation treatment, have provided a polarity stratigraphy of 12 pre-Pliocene magnetozones. Samples above 270 mbsf are of consistently high quality. Below this, magnetic behaviour is more variable. A preliminary age-depth plot using the Magnetic Polarity Time Scale (MPTS) and constrained by biostratigraphical data suggests that episodes of relatively rapid sedimentation took place at CRP-2 during Oligocene times (c. 100 m/My), but that more than half of the record was lost in a few major and many minor disconformities. Age estimates from Sr isotopes in shell debris and further tephra dating are expected to lead to a better comparison with the MPTS. CRP-2/2A has recorded a history of subsidence of the Victoria Land Basin margin that is similar to that found in CIROS-170 km to the south, reflecting stability in both basin and the adjacent mountains in late Cenozoic times, but with slow net accumulation in the middle Cenozoic. The climatic indicators from both drill holes show a similar correspondence, indicating polar conditions for the Quaternary but with sub-polar conditions in the early Miocene-late Oligocene and indications of warmer conditions still in the early Oligocene. Correlation between the CRP-2A core and seismic records shows that seismic units V3 and V4, both widespread in the Victoria Land Basin, represent a period of fluctuating ice margins and glacimarine sedimentation. The next drill hole, CRP-3, is expected to core deep into V5 and extend this record of climate and tectonics still further back in time.