Intimal proliferation and restenosis in paclitaxel-eluting stents with aminoparylene as carrier substance in swines

BACKGROUND: Polymer as carrier substance for drugeluting stents (DES) has been accused of inducing inflammation and hypersensitivity reactions leading to restenosis and stent thrombosis. Thus, a new paclitaxel-eluting stent (PES) with aminoparylene as a carrier substance is tested in the present study. METHODS: In 10 pigs, stents were implanted in the epicardial coronary arteries: 1) bare-metal stents (BMS, control stent); 2) cobalt-chromium stents (CCS); and 3) PES. Stent length was 15 mm, and diameter was 3 mm. The animals were restudied after 6 weeks. Quantitative coronary angiography was performed at baseline and follow up. Minimum luminal diameter (MLD) and late loss were calculated in all animals. Histologic vessel lumen, intimal proliferation and restenosis were determined by morphometry. Disruption of the lamina elastica interna (LEI) and inflammatory reactions were assessed by histology. RESULTS: The MLD at baseline was 2.83 +/- 0.28 mm, and at follow up it was 2.29 +/- 0.44 (p < 0.05; n = 30). Late loss and angiographic restenosis were smallest in the CCS and largest in the PES (ns). Neointimal proliferation was similar for all 3 stents, ranging between 1.38 and 1.64 mm(2) (ns). There was a significant correlation between disruption of the LEI and inflammatory reactions. CONCLUSIONS: PTs with aminoparylene as a carrier substance show similar late loss and angiographic restenosis to that of BM and CCS. The incidence of inflammatory reactions (35% of all histologic sections) is similar in all stents, but highest in PES. The mechanism of this reaction is unclear, but may be either due to the drug itself, the disruption of the LEI or to a hypersensitivity reaction.

Myocardial infarction due to paradoxical embolism in a patient with large atrial septal defect

We present the case of a patient who presented with acute inferior myocardial infarction and embolic occlusion of the distal left anterior descending and proximal right coronary artery. A large atrial septal defect (ASD) was seen on transesophageal echocardiography and the ASD was closed during the same session as coronary angiography and percutaneous coronary intervention. The presence of embolic or thrombotic occlusions of coronary arteries should prompt interventional cardiologists to look for a patent foramen ovale or ASD and perform percutaneous closure right away.

Differences in coronary artery plaques between target and non-target vessels

We used intravascular ultrasound (IVUS) and virtual histology (VH) to assess the differences of plaque burden and composition between target coronary arteries containing the culprit lesion and non-target coronary arteries.

Intravascular ultrasound-based left main coronary artery assessment: comparison between pullback from left anterior descending and circumflex arteries

We compared continuous pullback from the left anterior descending artery (LAD) with pullback from the circumflex artery (CX) for the assessment of the left main coronary artery (LMCA) by intravascular ultrasound (IVUS).

Na 1 Nachlass Max Horkheimer, 50 - Korrespondenzen u.a. an die Firma A. L. Stamm & Co (p. I 23, 190-421)

9 Briefe und Beilage zwischen Alfred Sohn-Rethel und Max Horkheimer, 1936-1940 sowie Briefwechsel mit Joan M. Levi; 6 Briefe zwischen Joan M. Levi und Max Horkheimer, 1940; 1 Brief von Max Horkheimer an Assistac Westcent, 25.06.1937; 1 Brief von John MacMurray an Walter Adams, 19.05.1937; 1 Brief von Walter Adams an Theodor W. Adorno, 01.06.1937; 2 Briefe zwischen Charles Somlo & Co und Max Horkheimer, 06.06.1939, 12.09.139; 1 Brief von Martin Sommerfeld an Max Horkheimer, 29.05.1934; 3 Briefe von Josef Sondek an Max Horkheimer, 1937, 1942; 3 Briefe zwischen Elsa Sontheimer, Max Sontheimer und Max Horkheimer, Februar 1940, 07.03.1940; 1 Drucksache von der The Southard School an Max Horkheimer; 1 Brief von der Soziologischen Verlagsanstalt an Gertrud Janosi, 20.07.1931; 9 Briefe zwsichen Maurice J. Speiser und Max Horkheimer, 1936-1948; 2 Briefe zwischen de Spengler und Max Horkheimer, 30.11.1936, 27.01.1937; 5 Briefe zwischen Sterling D. Spero und Max Horkheimer, 1936-1937; 1 Lebenslauf von Herbert Spielberg; 1 Brief und 2 Beilagen von René A. Spitz an Max Horkheimer, 23.06.1938; 2 Briefe von Elsa Spriesterbach an Max Horkheimer, Juli 1949; 1 Brief von Ida M. Stadie an Max Horkheimer, 21.05.1937; 20 Rechnungen von A. L. Stamm & Co an Max Horkheimer, 1938-1939; 1 Brief von Rose Horkheimer an A. L. Stamm und Co, 28.09.1938; 1 Betriebsanleitung und 1 Auslieferugnsschein für Max Horkheimer vom Standard Air Conditioning, 03.03.1936; 1 Brief von Max Horkheimer an Standard Air Conditioning, 28.03.1936; 5 Briefe zwischen Taylor Starck und Max Horkheimer, 1943; 8 Briefe zwischen Hans Staudinger und Max Horkheimer, 1937, 1943; 1 Briefauszug und Beilage von Paul Stefan, 1940 sowie Briefwechsel mit Samuel R. Wachtell; 1 Brief von Samuel R. Wachtell an Gertrude Blitz, 23.10.1940; 3 Briefe zwischen Leo Löwenthal und Samuel R. Wachtell, September 1940, 23.10.1940; 1 Brief von Loe Löwenthal an Hermann Kesten, 01.10.1940; 7 Briefe und Beilage zwischen George Stefansky und Max Horkheimer, 1939-1940; 2 Briefe zwischen dem Refugee Section of the American Friends Service Committee und Max Horkheimer, 16.05.1940, 28.05.1940; 3 Briefe zwischen dem Institute of International Education und Max Horkheimer, 09.04.1940, April 1940; 1 Brief von Max Horkheimer an Friess, 01.03.1940; 1 Brief vom Institute of Sociology Malvern und Max Horkheimer, 31.01.1940; 3 Briefe zwischen Stein und Max Horkheimer, 30.11.1934, 1936, 1937; 7 Briefe von Estell A. Stein an Max Horkheimer, 1929, 1937; 1 Brief von Franz Stein an Max Horkheimer; 1 Brief von Friedrich Pollock an Gertrude R. Stein, 22.03.1939; 1 Brief von Leo Stein an Max Horkheimer, 25.07.1944; 1 Brief von Max Horkheimer an Emilia Steinacher, 20.07.1937; 4 Briefe zwischen Friedrich Steinfeld und Max Horkheimer, 1941, 1945; 1 Brief und Beilage von Eugene G. Steinhof an Max Horkheimer; 3 Briefe zwischen Ernst Steinitz und Max Horkheimer, 25.04.1938, April 1938; 2 Briefe zwischen Theodor Steltzer und Eric E. Warburg, 07.03.1948; 4 Brief zwischen Hermine Sterler und Max Horkheimer, 11.09.1939, 1939, 1941; 4 Briefe zwischen Alfred K. Stern und Max Horkheimer, 1938, 1940 sowie 1 Brief und 1 Beilage von Max Gottschalk; 1 Brief von Max Gottschalk an Max Horkheimer; 2 Briefe und 1 Beilage zwischen Erich Stern und Max Horkheimer, 26.02.1937, 17.03.1937; 2 Briefe und Beilage von Eugene I. Stern an Max Horkheimer, 1938; 2 Briefe zwischen Joseph M. Weidberg und Max Horkheimer, 15.07.1938, 29.07.1938; 1 Brief von Max Horkheimer an das Cooperative Bureau for Teachers, 03.02.1938; 12 Briefe zwischen Günther Stern und Max Horkheimer, 1936, 1938 sowie Briefwechsel mit John Guggenheim Memorial Foundation; 3 Briefe und 1 Beilage zwischen der John Simon Guggenheim Memorial Foundation und Max Horkheimer, 1937; 1 Brief vom Social Research Quarterly an Max Horkheimer, 03.01.1937; 3 Briefe zwischen Hugo Stern und Max Horkheimer, 06.12.1937, Dezember 1937;

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).

Analyses of lake La Thuile sediment core

Lake La Thuile, in the Northern French Prealps (874 m a.s.l.), provides an 18 m long sedimentary sequence spanning the entire Lateglacial/Holocene period. The high resolution multi-proxy (sedimentological, palynological, geochemical) analysis of the uppermost 6.2 meters reveals the Holocene dynamics of erosion in the catchment in response to landscape modifications. The mountain belt is at relevant altitude to study past human activities and the watershed is sufficiently disconnected from large valleys to capture a local sedimentary signal. From 12,000 to 10,000 cal. BP (10 to 8 ka cal. BC), the onset of hardwood species triggered a drop in erosion following the Lateglacial/Holocene transition. From 10,000 to 4500 cal. BP (8 to 2.5 ka cal. BC), the forest became denser and favored slope stabilization while erosion processes were very weak. A first erosive phase was initiated at ca . 4500 cal. BP without evidence of human presence in the catchment. Then, the forest declined at approximately 3000 cal. BP, suggesting the first human influence on the landscape. Two other erosive phases are related to anthropic activities: approximately 2500 cal. BP (550 cal. BC) during the Roman period and after 1600 cal. BP (350 cal. AD) with a substantial accentuation in the Middle Ages. In contrast, the lower erosion produced during the Little Ice Age, when climate deteriorations are generally considered to result in an increased erosion signal in this region, suggests that anthropic activities dominated the erosive processes and completely masked the natural effects of climate on erosion in the late Holocene.

Grain size analyses, Ca/Ti and other selected elemental ratios from XRF core scanning of sediment cores from the Apulian Margin

An extensive, high-resolution, sedimentological-geochemical survey was done using geo-acoustics, XRF-core scans, ICP-AES, AMS 14C-dating and grain size analyses of sediments in 11 cores from the Gulf of Taranto, the southern Adriatic Sea, and the central Ionian Sea spanning the last 16 cal. ka BP. Comparable results were obtained for cores from the Gallipoli Shelf (eastern Gulf of Taranto), and the southern Adriatic Sea suggesting that the dominant provenance of Gallipoli Shelf sediments is from the western Adriatic mud belt. The 210Pb and 14C-dated high-accumulation-rate sediments permit a detailed reconstruction of climate variability over the last 16 cal. ka BP. Although, the Glacial-Interglacial transition is generally dry and stable these conditions are interrupted by two phases of increased detrital input during the Bølling-Allerød and the late Younger Dryas. The event during the Younger Dryas period is characterized by increased sediment inputs from southern Italian sources. This suggests that run-off was higher in southern- compared to northern Italy. At approximately ~ 7 cal. ka BP, increased detrital input from the Adriatic mud belt, related to sea level rise and the onset of deep water formation in the Adriatic Sea, is observed and is coincident with the end of sapropel S1 formation in the southern Adriatic Sea. During the mid-to-late Holocene we observed millennial-scale events of increased detrital input, e.g. during the Roman Humid Period, and of decreased detrital input, e.g., Medieval Warm Period. These dry/wet spells are consistent with variability in the North Atlantic Oscillation (NAO). A negative state of the NAO and thus a more advanced penetration of the westerlies into the central Mediterranean, that result in wet conditions in the research area concord with events of high detrital input e.g., during the Roman Humid Period. In contrast, a positive state of the NAO, resulting in dry conditions in the Mediterranean, dominated during events of rapid climate change such as the Medieval Warm Period and the Bronze Age.

Agricultural pesticide in sediment cores from the Lac de Saint-André, France

Agricultural pesticide use has increased worldwide during the last several decades, but the long-term fate, storage, and transfer dynamics of pesticides in a changing environment are poorly understood. Many pesticides have been progressively banned, but in numerous cases, these molecules are stable and may persist in soils, sediments, and ice. Many studies have addressed the question of their possible remobilization as a result of global change. In this article, we present a retro-observation approach based on lake sediment records to monitor micropollutants and to evaluate the long-term succession and diffuse transfer of herbicides, fungicides, and insecticide treatments in a vineyard catchment in France. The sediment allows for a reliable reconstruction of past pesticide use through time, validated by the historical introduction, use, and banning of these organic and inorganic pesticides in local vineyards. Our results also revealed how changes in these practices affect storage conditions and, consequently, the pesticides' transfer dynamics. For example, the use of postemergence herbicides (glyphosate), which induce an increase in soil erosion, led to a release of a banned remnant pesticide (dichlorodiphenyltrichloroethane, DDT), which had been previously stored in vineyard soil, back into the environment. Management strategies of ecotoxicological risk would be well served by recognition of the diversity of compounds stored in various environmental sinks, such as agriculture soil, and their capability to become sources when environmental conditions change.

Radiocarbon ages and average physical properties of sediment cores obtained during Icebreaker Oden cruise OSO0910

To date, understanding of ice sheet retreat within Pine Island Bay (PIB) following the Last Glacial Maximum (LGM) was based on seven radiocarbon dates and only fragmentary seafloor geomorphic evidence. During the austral summer 2009-2010, restricted sea ice cover allowed for the collection of 27 sediment cores from the outer PIB trough region. Combining these cores with data from prior cruises, over 133 cores have been used to conduct a detailed sedimentological facies analysis. These results, augmented by 23 new radiocarbon dates, are used to reconstruct the post-LGM deglacial history of PIB. Our results record a clear retreat stratigraphy in PIB composed of, from top to base; terrigenous sandy silt (distal glacimarine), pebbly sandy mud (ice-proximal glacimarine), and till. Initial retreat from the outer-continental shelf began shortly after the LGM and before 16.4 k cal yr BP, as a likely response to rising sea level. Bedforms in outer PIB document episodic retreat in the form of back-stepping grounding zone wedges and are associated with proximal glacimarine sediments. A sub-ice shelf facies is observed in central PIB and spans ~12.3-10.6 k cal yr BP. It is possible that widespread impingement of warm water onto the continental shelf caused an abrupt and widespread change from sub-ice shelf sedimentation to distal glacimarine sedimentation dominated by widespread dispersal of terrigenous silt between 7.8 and 7.0 k cal yr BP. The final phase of retreat ended before ~1.3 k cal yr BP, when the grounding line migrated to a location near the current ice margin.

Composition of suspended matter and bottom sediments from the North Dvina mouth area

Grain-size, mineral and chemical compositions of suspended particulate matter (SPM) from waters of the Severnaya (North) Dvina River mouth area during the spring flood in May 2004 is studied. Data published on composition of riverine SPM in the White Sea basin are very poor. The spring flood period when more than half of annual runoff is supplied from the river to the sea in during short time is understood more poorly. The paper considers comparison results of the grain size compositions of SPM and bottom sediments. Data of laser and hydraulic techniques of grain size analysis are compared. Short-period variations of SPM concentration and composition representing two diurnal peaks of the tide level are studied. It is found that SPM is mainly transferred during the spring flood as mineral aggregates up to 40 µm diameter. Sandy-silty fraction of riverine SPM settles in delta branches and channels, and bulk of clay-size material is supplied to the sea. Mineral and chemical compositions of SPM from the North Dvina River are determined by supply of material from the drainage basin. This material is subjected to intense mechanic separation during transfer to the sea. Key regularities of formation of mineral composition of SPM during the flood time are revealed. Effect of SPM grain size composition on distribution of minerals and chemical elements in study in the dynamic system of the river mouth area are characterized.

Accumulation rates and grain sizes of eolian dust in sediments of the Intertropical Convergence Zone in the northeast Pacific

A 328 cm-long piston core (KODOS 02-01-02) collected from the northeast equatorial Pacific at 16°12'N, 125°59'W was investigated for eolian mass fluxes and grain sizes to test these proxies as a tool for the paleo-position of the Intertropical Convergence Zone (ITCZ). The eolian mass fluxes of the lower interval below 250 cm (15.5-7.6 Ma) are very uniform at 5 +/- 1 mg/cm**2/kyr, while those of the upper interval above 250 cm (from 7.6 Ma) are over 2 times higher than the lower interval at 12 +/- 1 mg/cm**2/kyr. The median grain size of the eolian dusts in the lower interval increases from 8.4 Phi to 8.0 Phi downward, while that of the upper interval varies in a narrow range from 8.8 Phi to 8.6 Phi. The determined values compare well in magnitude to those of central Pacific sediments for the upper interval and equatorial and southeast Pacific sediments for the lower interval. This result suggests a possibility that the study site had been under the influence of southeast trade winds at its earlier depositional period due to the northerly position of the ITCZ, and subsequently of the northeast trade winds for a later period when the upper sediments were deposited. This interpretation is consistent with a mineralogical and geochemical study published elsewhere that assigned the provenance of the study core dust to Central/South America for the lower interval and to Asia for the upper interval. This study suggests that the distinct differences in eolian mass flux and grain size observed across the ITCZ can be used to trace the paleo-latitude of the ITCZ.