Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.However,crustal signatures in the mantle source of basaltic rocks above subduction zones were primarily incorporated in the form of...Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.However,crustal signatures in the mantle source of basaltic rocks above subduction zones were primarily incorporated in the form of liquid rather than solid phases.The physicochemical property of liquid phases is determined by the dehydration behavior of crustal rocks at the slab-mantle interface in subduction channels.Because of the significant fractionation in incompatible trace elements but the full inheritance in radiogenic isotopes relative to their crustal sources,the production of liquid phases is crucial to the geochemical transfer from the subducting crust into the mantle.In this process,the stability of specific minerals in subducting crustal rocks exerts a primary control on the enrichment of given trace elements in the liquid phases.For this reason,geochemically enriched oceanic basalts can be categorized into two types in terms of their trace element distribution patterns in the primitive mantle-normalized diagram.One is island arc basalts(IAB),showing enrichment in LILE,Pb and LREE but depletion in HFSE such as Nb and Ta relative to HREE,The other is ocean island basalts(OIB),exhibiting enrichment in LILE and LREE,enrichment or non-depletion in HFSE but depletion in Pb relative to HREE.In either types,these basalts show the enhanced enrichment of LILE and LREE with increasing their incompatibility relative to normal mid-ocean ridge basalts(MORB).The thermal regime of subduction zones can be categorized into two stages in both time and space,The first stage is characterized by compressional tectonism at low thermal gradients.As a consequence,metamorphic dehydration of the subducting crust prevails at forearc to subarc depths due to the breakdown of hydrous minerals such as mica and amphibole in the stability field of garnet and rutile,resulting in the liberation of aqueous solutions with the trace element composition that is considerably enriched in LILE,Pb and LREE but depleted in HFSE and HREE relative to normal M展开更多
AIM： To examine the effects of anti-high mobility group box 1 （HIGB1） neutralizing antibody in experimental severe acute pancreatitis （SAP）. METHODS： SAP was induced by creating closed duodenal loop inC3H/HeN mi...AIM： To examine the effects of anti-high mobility group box 1 （HIGB1） neutralizing antibody in experimental severe acute pancreatitis （SAP）. METHODS： SAP was induced by creating closed duodenal loop inC3H/HeN mice. SAP was induced immediately after intrapedtoneal injection of anti-HMGB1 neutralizing antibody （200 pg）. Sevedty of pancreatitis, organ injury （liver, kidney and lung）, and bacterial translocation to pancreas was examined 12 h after induction of SAP. RESULTS： Anti-HHGB1 neutralizing antibody significantly improved the elevation of the serum amylase level and the histological alterations of pancreas and lung in SAR Anti-HHGB1 antibody also significantly ameliorated the elevations of serum alanine aminotransferase and creatinine in SAR However, anti-HHGB1 antibody worsened the bacterial translocation to pancreas. CONCLUSION： Blockade of HHGB1 attenuated the development of SAP and associated organ dysfunction, suggesting that HHGB1 may act as a key mediator for inflammatory response and organ injury in SAR展开更多
基金supported by funds from the Chinese Academy of Sciences(XDB18020303)the Chinese Ministry of Science and Technology(2015CB856100)the National Natural ScienceFoundation of China(41590620)
文摘Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.However,crustal signatures in the mantle source of basaltic rocks above subduction zones were primarily incorporated in the form of liquid rather than solid phases.The physicochemical property of liquid phases is determined by the dehydration behavior of crustal rocks at the slab-mantle interface in subduction channels.Because of the significant fractionation in incompatible trace elements but the full inheritance in radiogenic isotopes relative to their crustal sources,the production of liquid phases is crucial to the geochemical transfer from the subducting crust into the mantle.In this process,the stability of specific minerals in subducting crustal rocks exerts a primary control on the enrichment of given trace elements in the liquid phases.For this reason,geochemically enriched oceanic basalts can be categorized into two types in terms of their trace element distribution patterns in the primitive mantle-normalized diagram.One is island arc basalts(IAB),showing enrichment in LILE,Pb and LREE but depletion in HFSE such as Nb and Ta relative to HREE,The other is ocean island basalts(OIB),exhibiting enrichment in LILE and LREE,enrichment or non-depletion in HFSE but depletion in Pb relative to HREE.In either types,these basalts show the enhanced enrichment of LILE and LREE with increasing their incompatibility relative to normal mid-ocean ridge basalts(MORB).The thermal regime of subduction zones can be categorized into two stages in both time and space,The first stage is characterized by compressional tectonism at low thermal gradients.As a consequence,metamorphic dehydration of the subducting crust prevails at forearc to subarc depths due to the breakdown of hydrous minerals such as mica and amphibole in the stability field of garnet and rutile,resulting in the liberation of aqueous solutions with the trace element composition that is considerably enriched in LILE,Pb and LREE but depleted in HFSE and HREE relative to normal M
基金Supported by Grants-in-Aid for Scientific Research from the Ministry of Education, Science, Sports and Culture of Japan and from the Ministry of Health, Labor and Welfare of Japan
文摘AIM： To examine the effects of anti-high mobility group box 1 （HIGB1） neutralizing antibody in experimental severe acute pancreatitis （SAP）. METHODS： SAP was induced by creating closed duodenal loop inC3H/HeN mice. SAP was induced immediately after intrapedtoneal injection of anti-HMGB1 neutralizing antibody （200 pg）. Sevedty of pancreatitis, organ injury （liver, kidney and lung）, and bacterial translocation to pancreas was examined 12 h after induction of SAP. RESULTS： Anti-HHGB1 neutralizing antibody significantly improved the elevation of the serum amylase level and the histological alterations of pancreas and lung in SAR Anti-HHGB1 antibody also significantly ameliorated the elevations of serum alanine aminotransferase and creatinine in SAR However, anti-HHGB1 antibody worsened the bacterial translocation to pancreas. CONCLUSION： Blockade of HHGB1 attenuated the development of SAP and associated organ dysfunction, suggesting that HHGB1 may act as a key mediator for inflammatory response and organ injury in SAR
