GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Keywords: Forschungsbericht ; Emitter ; Lithografie
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (22 Seiten, 4,88 MB) , Illustrationen, Diagramme
    Language: German
    Note: Förderkennzeichen BMWi 50RS1604 , Erscheinungsdatum dem Berichtsblatt entnommen. - Paralleltitel dem englischen Berichtsblatt entnommen , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of cutaneous pathology 24 (1997), S. 0 
    ISSN: 1600-0560
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: XMEL is a monoclonal antibody raised against part of the extracellular domain of the putative tyrosine kinase receptor protein implicated in the pathogenesis of melanoma formation in the Xiphophorus fish melanoma model. Our objective in this study was to determine the diagnostic and prognostic utility of XMEL for human melanoma. Formalin-fixed tissue from 82 melanomas, 42 carcinomas, 23 neural tumors, 12 lymphomas and 12 sarcomas were immunostained with XMEL and compared with a widely used melanoma antibody, HMB-45. The sensitivity of HMB-45 (83.1%) was similar to that of XMEL (79.8%). XMEL detected 7 melanomas that were HMB-45 negative. Specificity for detection of melanoma was greater with HMB-45 (95.5%) as compared to XMEL (80.9%). Of interest, all 4 prostatic adenocarcinomas were XMEL positive. These data suggest that XMEL is as sensitive but not as specific as HMB-45 in the detection of cutaneous melanoma but may serve as an ancillary antibody to improve diagnostic yield. The consistent positivity of XMEL in melanoma lends support to the hypothesis that the detected protein plays a role in melanoma pathogenesis. XMEL reactivity is not an independent prognosticator of death from melanoma in 37 melanomas from patients with at least 10 years' follow-up. These data and the fact that XMEL shows variable reactivity with metastatic melanomas but almost 100% reactivity with the primary melanomas suggest that the antigen recognized by the XMEL antibody may be important in the early stages of melanoma progression. This is supported by our earlier observation that XMEL is reactive with dysplastic nevi, a precursor of malignant melanoma.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Archives of dermatological research 194 (1952), S. 400-404 
    ISSN: 1432-069X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Zusammenfassung An rekonstituierten und nativen Kollagenfibrillen sowie an elastischen Fibrillen, die weitgehend frei von zelligen Bestandteilen und Kittsubstanzen präpariert waren, wurden Färbungen mit histologischen Farbstoffen und mit ph-Indikatorfarbstoffen vorgenommen. Dabei zeigten sich unerwartete Abweichungen in der Aufnahme von bekannten Farbstoffen. Diese Abweichungen müssen auf die Beeinflussung bzw. Beseitigung der Kittsubstanzen zurückgeführt werden. In einer Anzahl von Präparationen reagierten rekonstituierte Kollagenfibrillen, native Kollagenfibrillen und Elastinfibrillen gleichsinnig, so daß aus der Färbung allein keine Differenzierung möglich erschien. Versilberungen sind für Kollagen typisch und stellen echte Imprägnationen der Fasern dar. Einige Indikatorfarbstoffe gaben intensive metachromatische Färbungen. — Es wird auf die Bedeutung der angeführten Farbaufnahmeänderungen für pathologische Prozesse hingewiesen, die nach den Ergebnissen elektronenmikroskopischer Untersuchungen ohne Veränderungen des fibrillären Grundgerüstes vor sich gehen können, obwohl lichtmikroskopisch-histologisch eindeutige Veränderungen des Bindegewebes nach weisbar sind.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
  • 5
    Publication Date: 2024-02-07
    Description: Although subaqueous slopes on active continental margins are subject to a variety of failure styles, their movement mechanisms during earthquakes remain poorly constrained. A primary explanation is that few submarine landslides have been directly sampled for detailed investigation. We have conducted a series of dynamic shear experiments on samples recovered from the base of the Tuaheni Landslide Complex, located off the east coast of the North Island of New Zealand, to explore its behaviour during earthquakes. Our experiments suggest that whilst the basal landslide sediments can be prone to liquefaction in certain conditions, this is not a likely failure mechanism at the stress states operating in the low angled shear zone at the base of this landslide system. Instead, episodic landslide movement can occur through basal sliding when pore water pressures increase sufficiently to lower the shear zone effective stress to the material failure envelope. These low effective stress conditions are most likely to be reached during earthquakes that produce large amplitude, long duration ground shaking. The observed behaviour provides a credible mechanism through which subaqueous landslides moving on low angled shear zones in similar materials may be subject to episodic movement during earthquakes without undergoing catastrophic failure.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2024-02-07
    Description: Although submarine landslides have been studied for decades, a persistent challenge is the integration of diverse geoscientific datasets to characterise failure processes. We present a core-log-seismic integration study of the Tuaheni Landslide Complex to investigate intact sediments beneath the undeformed seafloor as well as post-failure landslide deposits. Beneath the undeformed seafloor are coherent reflections underlain by a weakly-reflective and chaotic seismic unit. This chaotic unit is characterised by variable shear strength that correlates with density fluctuations. The basal shear zone of the Tuaheni landslide likely exploited one (or more) of the low shear strength intervals. Within landslide deposits is a widespread “Intra-debris Reflector”, previously interpreted as the landslide’s basal shear zone. This reflector is a subtle impedance drop around the boundary between upper and lower landslide units. However, there is no pronounced shear strength change across this horizon. Rather, there is a pronounced reduction in shear strength ∼10-15 m above the Intra-debris Reflector that presumably represents an induced weak layer that developed during failure. Free gas accumulates beneath some regions of the landslide and is widespread deeper in the sedimentary sequence, suggesting that free gas may have played a role in pre-conditioning the slope to failure. Additional pre-conditioning or failure triggers could have been seismic shaking and associated transient fluid pressure. Our study underscores the importance of detailed core-log-seismic integration approaches for investigating basal shear zone development in submarine landslides.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2013-07-31
    Description: A bstract :— In marine environments, sediments from different sources are stirred and dispersed, generating beds that are composed of mixed and layered sediments of differing grain sizes. Traditional engineering formulations used to predict erosion thresholds are however, generally for unimodal sediment distributions, and so may be inadequate for commonly occurring coastal sediments. We tested the transport behavior of deposited and mixed sediment beds consisting of a simplified two-grain fraction (silt (D 50 = 55 µm) and sand (D 50 = 300 µm)) in a laboratory-based annular flume with the objective of investigating the parameters controlling the stability of a sediment bed. To mimic recent deposition of particles following large storm events and the longer-term result of the incorporation of fines in coarse sediment, we designed two suites of experiments: (1) "the layering experiment": in which a sandy bed was covered by a thin layer of silt of varying thickness (0.2–3 mm; 0.5–3.7 wt %, dry weight in a layer 10 cm deep); and (2) "the mixing experiment" where the bed was composed of sand homogeneously mixed with small amounts of silt (0.07–0.7 wt %, dry weight). To initiate erosion and to detect a possible stabilizing effect in both settings, we increased the flow speeds in increments up to 0.30 m/s. Results showed that the sediment bed (or the underlying sand bed in the case of the layering experiment) stabilized with increasing silt composition. The increasing sediment stability was defined by a shift of the initial threshold conditions towards higher flow speeds, combined with, in the case of the mixed bed, decreasing erosion rates. Our results show that even extremely low concentrations of silt play a stabilizing role (1.4% silt (wt %) on a layered sediment bed of 10 cm thickness). In the case of a mixed sediment bed, 0.18% silt (wt %, in a sample of 10 cm depth) stabilized the bed. Both cases show that the depositional history of the sediment fractions can change the erosion characteristics of the seabed. These observations are summarized in a conceptual model that suggests that, in addition to the effect on surface roughness, silt stabilizes the sand bed by pore-space plugging and reducing the inflow in the bed, and hence increases the bed stability. Measurements of hydraulic conductivity on similar bed assemblages qualitatively supported this conclusion by showing that silt could decrease the permeability by up to 22% in the case of a layered bed and by up to 70% in the case of a mixed bed.
    Print ISSN: 1527-1404
    Topics: Geosciences
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2014-12-03
    Description: Yakun Xie, Kerstin Huhn, Ronny Brandt, Maren Potschin, Stefan Bieker, Daniel Straub, Jasmin Doll, Thomas Drechsler, Ulrike Zentgraf, and Stephan Wenkel As sessile organisms, plants have to continuously adjust growth and development to ever-changing environmental conditions. At the end of the growing season, annual plants induce leaf senescence to reallocate nutrients and energy-rich substances from the leaves to the maturing seeds. Thus, leaf senescence is a means with which to increase reproductive success and is therefore tightly coupled to the developmental age of the plant. However, senescence can also be induced in response to sub-optimal growth conditions as an exit strategy, which is accompanied by severely reduced yield. Here, we show that class III homeodomain leucine zipper (HD-ZIPIII) transcription factors, which are known to be involved in basic pattern formation, have an additional role in controlling the onset of leaf senescence in Arabidopsis . Several potential direct downstream genes of the HD-ZIPIII protein REVOLUTA (REV) have known roles in environment-controlled physiological processes. We report that REV acts as a redox-sensitive transcription factor, and directly and positively regulates the expression of WRKY53 , a master regulator of age-induced leaf senescence. HD-ZIPIII proteins are required for the full induction of WRKY53 in response to oxidative stress, and mutations in HD-ZIPIII genes strongly delay the onset of senescence. Thus, a crosstalk between early and late stages of leaf development appears to contribute to reproductive success.
    Print ISSN: 0950-1991
    Electronic ISSN: 1477-9129
    Topics: Biology
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2019-07-16
    Description: Seismic profiles extending from the southern South African shelf into the deep sea reveal a strong erosional activity, which affects large parts of the continental margin. Recent to Oligocene sequences, and in places the whole sedimentary column, appear to have been removed. Mass movements were considered as the origin of this erosion. However, structures indicating slumping could only be identified in a few places, The erosional activity is confined to specific water depths, which correlate well with the activity levels of water masses observed here. We thus suggest that the Agulhas Current, Antarctic Intermediate Water, North Atlantic Deep Water, and Antarctic Bottomwater have intensively shaped the sedimentary sequences for a considerable period. It is difficult to estimate the duration of the erosion. Numerical simulation of sediment transport and erosion is needed to indicate the onset of the erosional activity.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2019-07-16
    Description: Der interozeanische Austausch der Wassermassen südlich von Südafrika ist für die globale thermohaline Zirkulation von zentraler Bedeutung. Zunahme oder Abschwächung dieses Wassermassenaustausches führen zur Verstärkung oder Abschwächung der atlantischen Umwälzbewegung sowie zu einer entsprechenden Veränderung der Tiefenwasserbildung im Nordatlantik. Während der FS SONNE Fahrt SO-182 im April-Mai 2005 wurden mehr als 2800 Kilometer hoch auflösende refexionsseismische Daten im Transkei Becken südöstlich von Südafrika gemessen. Die Analyse zeigt, dass Nordatlantisches Tiefenwasser (NADW) und Antarktisches Bodenwasser (AABW) die Sedimentbildung in dieser Region stark beeinflussen. Die Beobachtungen zeigen weiter, dass die Ströme in dieser Region sehr variabel waren: Eine Nord-Süd-Strömung von AABW beherrschte Sedimenttransport und -absetzung im Transkei Becken vom mittlerem Miozän bis zum frühen Pliozän, gefolgt von einem Haupttransport in W-E Richtung durch NADW. Um die Sedimentanordnung und die Entwicklung der Paläozirkulation südlich von Südafrika besser zu verstehen, wird ein Ozeanzirkulationsmodell benutzt, das mit einem Sedimentmodell gekoppelt ist.Das eingesetzte Modell ist das Regional Ocean Modeling System (ROMS), das auf hydrostatischen, primitiven Gleichungen basiert. Es nutzt terrainfolgende Koordinaten in der Vertikalen und orthogonal gekrümmte Koordinaten in der Horizontalen, die je nach Fragestellung unterschiedliche Auflösung haben. Das Modell simuliert das gegenwärtige Strömungssystem in der Region südlich von Südafrika. Basierend auf dem Modell wird die Simulation der regionalen Verteilung von Sand und Silt weiterentwickelt.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...