The Moxee City (Washington) Mammoth: Morphostratigraphic, Taphonomic, and Taxonomic Considerations

A nearly complete, but highly fractured, proboscidean tusk was unearthed during parking lot construction near Moxee City in central Washington in May 2001. Schreger angle analysis revealed that the tusk was from a mammoth. AMS radiocarbon dating of the tusk established that the mammoth died 14,570 14C yr BP. The age, combined with the biogeography of proboscidean finds in the Pacific Northwest, suggests the tusk is from a Columbian mammoth (Mammuthus columbi). The condition of the tusk and its association with basalt and crystalline erratics suggest that a locally derived tusk was swept up in the advancing flood and transported to ∼320 m elevation, where it was deposited in the sediments of the 3rd of 3 Missoula Floods that are preserved in the area. The tusk\u27s weathering indicates subaerial exposure prior to burial in the slackwater sediments. Slackwater deposits at the site are pale, ∼30-100 cm thick, calcareous, fine-textured strata that include occasional coarse basalt and crystalline sand and gravel. They are intruded by numerous clastic dikes. The sediments encapsulating the tusk lack rhythmites because of their deposition in the nearshore zone of an ephemeral slackwater lake. The first 2 floods inundated the site between 15,300 14C yr BP and 14,570 14C yr BP, stripping the A horizon from a well-developed soil formed in alluvial fan sediments sitting above an Ellensburg Formation pediment. The last flood to reach the site occurred later than 14,570 14C yr BP, as indicated by the presence of the dated tusk. Post-flood and post-MSH S tephra loess derived from the Yakima River floodplain mantles these slackwater deposits. The Warden soil is forming in the now-stable loess parent material

Kolsänkan av levande biomassa i fjällnära skog

The study focuses on facts about the role of the forests, near the mountains in the northwestern part of Sweden, from a climate perspective. This refers to the net removal in living tree biomass while the substitution effect is omitted. The area-based (design based) estimates are based on data from the Swedish National Forest Inventories permanent sample plots in two areas close to the mountains. The first area refers to the above limit for forests close to the mountains (above GFS) according to the Swedish Forest Agency and the second according to a map layer that is considered important of protection for biodiversity reasons according to the Swedish Environmental Protection Agency (SEPA). Of the 8.1 Mha of land above the limit for forests close to mountains, 3.1 Mha is forest land, of which 1.7 Mha is formally protected forest land. Productive forest land used for timber production amounts to less than 0.5 Mha. For both formally protected forest land and non-formally protected forest land, living biomass constitutes a net uptake of -1 Mton CO2 / year during the period 1990-2016 on a reasonably similar area. If all forest land above GFS is excluded from timber production, the short-term increase in net removal in the forest will be approximately -0.4 Mton CO2 / year, which corresponds to harvest. Then we do not expect any substitution effect and believe that other carbon pools (dead wood, soil, litter and the carbon pool harvested wood products) in the short term are not affected by the stopping of felling. The Swedish Environmental Protection Agency has selected an area close to the mountains where two thirds comprise forest land. No land is formally protected. Of approximately 1.0 Mha of forest land, 0.39 Mha was assessed as forest land for timber production. The net uptake in living biomass of forest land amounted to approximately -1 Mton CO2 / year during the period. On productive forest land for timber production, the net uptake was approximately -0.6 Mton CO2 / year during the period. If all forest land according to the map layer is excluded from timber production, the short-term increase in net removal in the forest will be approximately -0.1 Mton CO2 / year, which corresponds to harvest. Then we do not expect any substitution effect and believe that other carbon pools in the short term are not affected by the stopping of felling.The study focuses on facts about the role of the forests, near the mountains in the northwestern part of Sweden, from a climate perspective. This refers to the net removal in living tree biomass while the substitution effect is omitted. The area-based (design based) estimates are based on data from the Swedish National Forest Inventories permanent sample plots in two areas close to the mountains. The first area refers to the above limit for forests close to the mountains (above GFS) according to the Swedish Forest Agency and the second according to a map layer that is considered important of protection for biodiversity reasons according to the Swedish Environmental Protection Agency (SEPA). Of the 8.1 Mha of land above the limit for forests close to mountains, 3.1 Mha is forest land, of which 1.7 Mha is formally protected forest land. Productive forest land used for timber production amounts to less than 0.5 Mha. For both formally protected forest land and non-formally protected forest land, living biomass constitutes a net uptake of -1 Mton CO2 / year during the period 1990-2016 on a reasonably similar area. If all forest land above GFS is excluded from timber production, the short-term increase in net removal in the forest will be approximately -0.4 Mton CO2 / year, which corresponds to harvest. Then we do not expect any substitution effect and believe that other carbon pools (dead wood, soil, litter and the carbon pool harvested wood products) in the short term are not affected by the stopping of felling. The Swedish Environmental Protection Agency has selected an area close to the mountains where two thirds comprise forest land. No land is formally protected. Of approximately 1.0 Mha of forest land, 0.39 Mha was assessed as forest land for timber production. The net uptake in living biomass of forest land amounted to approximately -1 Mton CO2 / year during the period. On productive forest land for timber production, the net uptake was approximately -0.6 Mton CO2 / year during the period. If all forest land according to the map layer is excluded from timber production, the short-term increase in net removal in the forest will be approximately -0.1 Mton CO2 / year, which corresponds to harvest. Then we do not expect any substitution effect and believe that other carbon pools in the short term are not affected by the stopping of felling

The Scandinavian multicenter hemodynamic evaluation of the SJM Regent aortic valve

Background: 112 patients who received small and medium sized St.Jude Regent heart valves (19-25 mm) at 7 Scandinavian centers were studied between January 2003 and February 2005 to obtain non-invasive data regarding the hemodynamic performance at rest and during Dobutamine stress echocardiography (DSE) testing one year after surgery. Material and methods: 46 woman and 66 men, aged 61.8 +/- 9.7 (18-75) years, were operated on for aortic regurgitation (17), stenosis (65), or mixed dysfunction (30). Valve sizes were 19 mm (6), 21 mm (33), 23 mm (41), 25 mm (30). Two patients receiving size 27 valves were excluded from the hemodynamic evaluation. Pledgets were used in 100 patients, everted mattress in 66 and simple interrupted sutures in 21. Valve orientation varied and was dependent on the surgeons' choice. 34 patients (30.4%) underwent concomitant coronary artery surgery. Results: There were two early deaths (1.8%) and three late deaths, one because of pancreatic cancer. Late events during follow-up were: non structural dysfunction (1), bleeding (2), thromboembolism (2). At one year follow up 93% of the patients were in NYHA classes 1-2 versus 47.8% preoperatively. Dobutamine stress echocardiography (DSE) was performed in a total of 66 and maximal peak stress was reached in 61 patients. During DSE testing, the following statistically significant changes took place: Heart rate increased by 73.0%, cardiac output by 85.5%, left ventriclular ejection fraction by 19.6%, and maximal mean prosthetic transvalvular gradient by 133.8%, whereas the effective orifice area index did not change. Left ventricular mass fell during one year from 215 +/- 63 to 197 +/- 62 g (p < 0.05). Conclusion: The Dobutamine test induces a substantial stress, well suitable for echocardiographic assessment of prosthesis valve function and can be performed in the majority of the patients. The changes in pressure gradients add to the hemodynamic characteristics of the various valve sizes. In our patients the St. Jude Regent valve performed satisfactory at rest and under pharmacological stress situation

Mitral valve analysis adding a virtual semi-transparent annulus plane for detection of prolapsing segments

Background We hypothesized that a novel three-dimensional virtual semi-transparent annulus plane (3D VSAP) presented on a holographic screen can be used to visualize the prolapsing tissue in degenerative mitral valve disease and furthermore, provide us with geometrical data of the mitral valve apparatus. Phantom and patient studies were designed to demonstrate the feasibility of creating a semi-automatic, semi-transparent mitral annulus plane visualized on a holographic display. Methods Ten pipe cleaners mimicking the mitral annulus with different shapes and three types of annuloplasty rings served as phantoms. We obtained 3D transoesophageal examination of the phantoms in a special designed box filled with water. Recordings were converted to the holographic display and a 3D VSAP was created. The ratio of the major and minor axes as well as the non-planar angles were calculated and compared with direct measures of the phantoms. Forty patients with degenerative mitral valve disease were then analyzed with 3D transthoracic echocardiography (TTE) and a 3D VSAP was created on the holographic display. A total of 240 segments were analyzed by two independent observers, one echo expert (observer I), and the other novice with limited echo experience (observer II). The two observers created the 3D VSAP in each patient before suggesting the valve pathology. Results The major/minor axes ratio and non-planar angles by 3D VSAP correlated with direct measurements by r = 0.65, p < 0.02 and r = 0.99, p < 0.0001, respectively. The sensitivity and specificity of the 3D VSAP method in patients was 81 and 97 %, respectively (observer I) and for observer II 77 and 96 %, respectively. The accuracy and precisions were 93.9 and 89.4 %, respectively (observer I), 92.3 and 85.1 % (observer II). Mitral valve analysis adding a 3D VSAP was feasible with high accuracy and precision, providing a quick and less subjective method for diagnosing mitral valve prolapse. This novel method may improve preoperative diagnostics and may relieve a better understanding of the pathophysiology of mitral valve disease. Thus, based on the specific findings in each patient, a tailored surgical repair can be planned and hopefully enhance long-term repair patency in the future

ABS-NET: Fully Decentralized Runtime Adaptation for Distributed Objects

We present a formalized, fully decentralized runtime semantics for a core subset of ABS, a language graph representation of a network infrastructure, with network endpoints represented as graph nodes, and links as arcs with buffers, corresponding to OSI layer 2 interconnects. The key problem we wish to address is how to allocate computational tasks to nodes so that certain performance objectives are met. To this end, we use the semantics as a foundation for performing networkadaptive task execution via object migration between nodes. Adaptability is analyzed in terms of three Quality of Service objectives: node load, arc load and message latency. We have implemented the key parts of our semantics in a simulator and evaluated how well objectives are achieved for some application-relevant choices of network topology, migration procedure and ABS program. The evaluation suggests that it is feasible in a decentralized setting to continually meet both the objective of a node-balanced task allocation and make headway towards minimizing communication, and thus arc load and message latency.

Skattning av areal organogen mark för alla ägoslag

Torvmark lagrar stora mängder organiskt kol som kan emitteras i samband med brukande. Vidare kan lustgas och metan släppas ut från torvmark och därför anses variabeln viktig ur ett klimatperspektiv. Vi har valt att definiera torvmark som att ”mer än halva arealen täcks av torv”. Riksskogstaxeringen har en mer detaljerad definition men normalt ska torvlagret vara djupare än 30 cm. Riksskogstaxeringen mäter alltid torvmark på ägoslagen Skogsmark, Naturbete, Myr, Fjällbarrskog och Annat klimatimpediment (men periodvis har mätningar även förekommit på andra ägoslag). Därmed saknas variabeln för vissa ägoslag. Om provytan är delad i mer än ett ägoslag mäts variabeln per delyta. Internt i nuvarande klimatrapportering redovisas torvmark utifrån en inventering per omdrev (2003-2007) fast variabeln registreras vid varje återinventering av samma provyta. Tanken är att undvika variation orsakad av personlig bedömning i fält samtidigt som vi tror att variabeln sällan ändras. Det finns nu en möjlighet att grovt komplettera variabeln torvmark för ägoslag där densamma inte registrerats av Riksskogstaxering. Tanken är att använda SGUs jordartskarta för ändamålet. Uppgiften går ut på att komplettera de provytor som saknar bedömning av variabeln torvmark med uppgifter från ett nyproducerat kartskikt. Vidare kommer en kontinuerlig registrering av variabeln torvmark per inventeringstillfälle vägas mot att, som idag, enbart basera mätningen på ett inventeringstillfälle