Geomorphological and sedimentary evidence for late Pleistocene to Holocene hydrological change along the Río Mamoré, Bolivian Amazon

Aerial photography and satellite imagery reveal manifold geomorphological evidence of a dynamic evolution of past and present rivers in the Bolivian Amazon. Comparison of oxbow lake and meander scar dimensions along an inactive meander belt of the Río Mamoré (Llanos de Moxos, north-eastern Bolivia) and its modern counterpart suggests significant regional paleohydrological variability. We used these features as geomorphological and sedimentary archives to enhance our understanding of longer-term variations of the fluvial system. Late Pleistocene to Holocene hydrological changes of the Río Mamoré are inferred from: (i) the analysis of satellite imagery, (ii) discharge estimates from meander morphology, (iii) stratigraphic, and (iv) chronological information based on luminescence and radiocarbon dating. The combined data from three oxbows indicate that the now abandoned meander belt – the paleo-Mamoré – continued to be active at least until ∼5 ka, and likely even postdating 3 ka. An up to threefold increase in discharge is estimated for the modern Río Mamoré versus the paleo-Mamoré. The altered runoff regime may have triggered an avulsive shift towards the currently active Río Mamoré. The preceding increase in discharge in turn, was possibly related to a shift in climatic conditions, which changed markedly between the mid- and late Holocene in tropical South America. In addition, it may have been the indirect result of capturing the avulsive Río Grande system to the east of the Río Mamoré. Alternative explanations for the differences in dimensions of the paleo versus the modern Río Mamoré, i.e. contemporaneous activity of both rivers or alteration of site factors such as the channel/floodplain relationship, are considered to be unlikely.

Microsurgical treatment of perimedullary spinal arteriovenous fistulas

Objective: Perimedullary arteriovenous fistulas (PMAVF) are exceptional spinal vascular malformations and their best therapeutic management remains controversial. Here the authors present their experience with PMAVF to characterize the clinical, neuroimaging and treatment data of patients operated on PMAVF and to analyse both incidence of complications and resurgery in the microsurgical therapy of PMAVF. Method: Fifteen patients (13 men, 2 women, mean age 51 years) with PMAVF identified by selective spinal angiography were microsurgically treated at our institution between 1992 and 2006. The presenting symptoms (duration 3 months to 5 years) were consistent with progressive myelopathy (13) or included isolated pain syndrome (2). Lumbar PMAVF location (6) was predominant followed by the sacral (5) and thoracic (4) site including 6 PMAVF of the filum terminale and 2 PMAVF associated with a glomerular AVM and dural arteriovenous fistula, respectively. Microsurgical PMAVF obliteration and postoperative angiography were routinely performed. All patients were available for follow-up evaluation within 6 months postoperatively. Results: Surgery with complete (12) or almost complete (3) PMAVF occlusion resulted in neurological improvement (10) or stabilization (1), 4 patients deteriorated postoperatively. Whereas no complications occured, a second operation because of residual or recanalized PMAVF was indicated in one case each. Two associated dual spinal vascular malformations could be observed and subsequently obliterated. Conclusions: Microsurgical occlusion of PMAVF appears to be a secure and adequate therapeutic option that prevents progressive neurological deterioration and results in good outcome in the majority of patients. Complications associated with surgery, recurrences and reoperations are infrequent. Therefore, in the authors experience microsurgery is the preferred therapy to treat PMAVF. Despite the rarity of PMAVF the possibility of the coincidence of associated second vascular malformations should be considered.

The origin of oriented lakes: evidence from the Bolivian Amazon

The presence of hundreds of rectangular and oriented lakes is one of the most striking characteristics of the Llanos de Moxos (LM) landscape in the Bolivian Amazon. Oriented lakes also occur in the Arctic coastal plains of Russia, Alaska and Canada and along the Atlantic Coastal Plain from northeast Florida to southeast New Jersey and along the coast of northeast Brazil. Many different mechanisms have been proposed for their formation. In the LM, Plafker's (1964) tectonic model, in which subsidence results from the propagation of bedrock faults through the foreland sediments, is the most accepted. However, this model has not been verified. Here, we present new results from stratigraphic transects across the borders of three rectangular and oriented lakes in the LM. A paleosol buried under mid-Holocene sediments is used as a stratigraphic marker to assess the vertical displacement of sediments on both sides of the alleged faults. Our results show that there is no vertical displacement and, therefore, that Plafker's model can be ruled out. We suggest that, among all the proposed mechanisms behind lake formation, the combined action of wind and waves is the most likely. The evidence from the LM provides new hints for the formation of oriented lakes worldwide.

Geomorphology and evolution of the late Pleistocene to Holocene fluvial system in the south-eastern Llanos de Moxos, Bolivian Amazon

In the Bolivian Amazon several paleochannel generations are preserved. Their wide spectrum of morphologies clearly provides crucial information on the type and magnitude of geomorphic and hydrological changes within the drainage network of the Andean foreland. Therefore, in this study we mapped geomorphological characteristics of paleochannels, and applied radiocarbon and optically stimulated luminescence dating. Seven paleochannel generations are identified. Significant changes in sinuosity, channel widths and river pattern are observed for the successive paleochannel generations. Our results clearly reflect at least three different geomorphic and hydrological periods in the evolution of the fluvial system since the late Pleistocene. Changes in discharge and sediment load may be controlled by combinations of two interrelated mechanisms: (i) spatial changes and re-organizations of the drainage network in the upper catchment, and/or (ii) climate changes with their associated local to catchment-scale modifications in vegetation cover, and changes in discharge, inundation frequencies and magnitudes, which have likely affected the evolution of the fluvial system in the Llanos de Moxos. In summary, our study has revealed the enormous potential which geomorphic mapping and analysis combined with luminescence based chronologies hold for the reconstruction of the late Pleistocene to recent fluvial system in a large portion of Amazonia.

Clinical experience with the freedom SOLO stentless aortic valve in 277 consecutive patients.

BACKGROUND The Sorin Freedom SOLO (FS) bovine pericardial stentless valve prosthesis is designed for supraannular, subcoronary implantation. We report our experience and results with 277 consecutively implanted FS bioprostheses. METHODS 277 patients (mean age, 74.2 ± 7.3 years; 139 (50.2%) female) underwent aortic valve replacement (AVR) with the FS stentless bioprosthesis. The hemodynamic performance was investigated with transthoracic echocardiography at discharge, 6 months later, and yearly thereafter. Follow-up was 100% complete, with an average observation time of 2.6 ± 1.7 years and a total of 697.3 patient-years. RESULTS The overall 30-day mortality was 4.3%. The mortalities for isolated AVR and combined procedures were 1.9% and 7.3%, respectively. No causes of death were valve-related. Preoperative peak (74.2 ± 23.0 mm Hg) and mean (48.6 ± 16.3 mm Hg) gradients decreased to 15.6 ± 5.4 mm Hg and 8.8 ± 3.0 mm Hg postoperatively and remained unchanged for as long as 5 years. The postoperative mean effective orifice area (EOA) for valve sizes 19, 21, 23, 25, and 27 were 1.49 ± 0.32 cm(2), 1.67 ± 0.40 cm(2), 1.92 ± 0.38 cm(2), 2.01 ± 0.42 cm(2), and 2.13 ± 0.36 cm(2), respectively. Severe prosthesis-patient mismach (PPM) was completely absent, and moderate PPM occurred in 17 patients (6.1%). In isolated AVR, 0.8% of patients with preoperative sinus rhythm required a permanent pacemaker before hospital discharge. There was 100% freedom from structural valve deterioration, 99.6 % freedom from endocarditis and reoperation, and 97.3% freedom from thromboembolism at 5 years. CONCLUSIONS The FS stentless aortic valve is safe to implant, and it shows excellent hemodynamic performance and early and midterm results. Owing to the favorable EOA, the valve appears particularly attractive for patients at risk for PPM.

Intravitreal ranibizumab monotherapy to treat retinopathy of prematurity zone II, stage 3 with plus disease.

BACKGROUND Treatment of retinopathy of prematurity (ROP) stage 3 plus with bevacizumab is still very controversial. We report the outcome of 6 eyes of 4 premature infants with ROP stage 3 plus disease treated with ranibizumab monotherapy. METHODS Six eyes of 4 premature infants with threshold ROP 3 plus disease in zone II, were treated with one intravitreal injection of 0.03 ml ranibizumab. No prior laser or other intravitreal therapy was done. Fundus examination was performed prior to the intervention and at each follow-up visit. Changes in various mean vital parameters one week post intervention compared to one week pre-intervention were assessed. RESULTS The gestational age (GA) of patient 1, 2, 3, and 4 at birth was 24 5/7, 24 5/7, 24 4/7, and 26 1/7 weeks, respectively. The birth weight was 500 grams, 450 grams, 665 grams, and 745 grams, respectively. The GA at the date of treatment ranged from 34 3/7 to 38 6/7 weeks. In one infant, upper air way infection was observed 2 days post injection of the second eye. Three eyes required paracentesis to reduce the intraocular pressure after injection and to restore central artery perfusion. After six months, all eyes showed complete retinal vascularisation without any signs of disease recurrence. CONCLUSIONS Treatment of ROP 3 plus disease with intravitreal ranibizumab was effective in all cases and should be considered for treatment. One infant developed an upper air way infection suspicious for nasopharyngitis, which might be a possible side effect of ranibizumab. Another frequent complication was intraocular pressure rise after injection. More patients with longer follow-up duration are mandatory to confirm the safety and efficacy of this treatment. TRIAL REGISTRATION NUMBER NCT02164604 ; Date of registration: 13.06.2014.

Landscape Transformation and Sustainable Development in Ethiopia: Background information for a study tour through Ethiopia, 4-20 September 2006

This report presents background material used by participants in a joint Ethiopian-Swiss study tour through the north-central highlands of Ethiopia. The main theme of the tour was 'land transformation and sustainable development'. The tour took place from 4-20 September 2006, starting in Addis Abeba and continuing through North Shewa, Wello, Gonder and Gojam. This report is a structured compilation of information gathered by MSc candidates and scientists from the University of Bern prior to the study tour, and supplemented with daily reports by all participants after the study tour was completed.

Long-term man–environment interactions in the Bolivian Amazon: 8000 years of vegetation dynamics

Only few studies documenting the vegetation history of the Llanos de Moxos, one of the largest seasonally flooded wetland areas in South America, are available and little is known about the environmental impact of pre-Columbian settlements. We use radiocarbon-dated terrestrial plant macrofossils to establish a sound chronology and palynological analyses to reconstruct the vegetation and fire history of the Lago Rogaguado area. The sedimentary pollen and spore record suggests that wetland and wooded savannah (Cerrado) environments occurred around the lake between 8100 and 5800 cal BP. Fire activity was high during this period and was probably connected to the dry Cerrado environments. The pollen evidence suggests early plant cultivation (Zea mays, Annonaceae and Cucurbitaceae) from 6500 cal BP onwards, which is significantly earlier than hitherto assumed for Amazonia. Gallery forests expanded after 5800 cal BP, when fire activity strongly declined. Forest expansion intensified around 2800 cal BP and continued until 2000 cal BP, when forest cover reached its maximum and fire activity its minimum. The late-Holocene forest expansion to the south and the decrease of fire activity may have resulted from a climatic shift to moister conditions (possibly a shorter dry season). New crops (e.g. Avena-type) or adventive plants (e.g. Rumex acetosella-type) document the impact of European economies after ca. 500 cal BP. Land use intensity remained rather stable over the most recent centuries, arguing against a collapse of settlements in response to the arrival of Europeans, as reconstructed from other Amazonian pollen records.