Chickpea(Cicer arietinum L.) and pigeonpea [Cajanus cajan L.(Millsp.)] play an important role in mitigating protein malnutrition for millions of poor vegetarians living in regions of the semi-arid tropics. Abiotic str...Chickpea(Cicer arietinum L.) and pigeonpea [Cajanus cajan L.(Millsp.)] play an important role in mitigating protein malnutrition for millions of poor vegetarians living in regions of the semi-arid tropics. Abiotic stresses such as excess and limited soil moisture(water-logging and drought), heat and chilling(high and low temperature stresses), soil salinity, and acidity are major yield constraints, as these two crops are grown mostly under rainfed conditions in risk-prone marginal and degraded lands with few or no inputs. Losses due to such stresses vary from 30% to 100% depending on their severity. The literature abounds in basic information concerning screening techniques, physiological mechanisms, and genetics of traits associated with resistance/tolerance to abiotic stresses in these two crops. However, the final outcome in terms of resistant/tolerant varieties has been far from satisfactory. This situation calls for improving selection efficiency through precise phenotyping and genotyping under high-throughput controlled conditions using modern tools of genomics. In this review, we suggest that an integrated approach combining advances from genetics, physiology, and biotechnology needs to be used for higher precision and efficiency of breeding programs aimed at improving abiotic stress tolerance in both chickpea and pigeonpea.展开更多
The amphibolites from the Mauranipur and Babina regions are located in the central part of the Bundelkhand Craton(BuC),northern India.During the geodynamic evolution of the BuC,these amphibolites underwent medium-grad...The amphibolites from the Mauranipur and Babina regions are located in the central part of the Bundelkhand Craton(BuC),northern India.During the geodynamic evolution of the BuC,these amphibolites underwent medium-grade metamorphism.This study combines textural observations of amphibolites from two distinct regions(Mauranipur and Babina)with mineral chemistry and phase equilibrium modelling.Observations suggest that the amphibolites of both areas have gone through three stages of metamorphism.The pre-peak stage in the amphibolites from the Mauranipur and Babina regions is marked by the assemblages Ep-Amp-Cpx-Pl-Ilm-Ru-Qz and Ep-Amp-Cpx-Pl-Ab-Ilm-Qz respectively;the peak metamorphic stage is characterized by the mineral assemblages Amp-Cpx-Pl-Ilm-Ru-Qz and Amp-Cpx-Pl-Ilm-Qz-H_(2)O,which is formed during the burial process,and the post-peak stage is represented by the assemblages Amp-Pl-Ilm-Ru-Qz and Amp-Pl-Ilm-Qz-H_(2)O respectively,which is formed by exhumation event.By applying the phase equilibria modelling in the NCFMASHTO system,the P-T conditions estimated from pre-peak,peak to post-peak stages are characterized as 6.7 kbar/510 oC,7.3 kbar/578ºC and>3.0 kbar/>585ºC,respectively,for the Mauranipur amphibolites;and 6.27 kbar/520ºC,5.2 kbar/805ºC and>3.0 kbar/>640ºC respectively for Babina amphibolites.The textural association and P-T conditions of both amphibolites suggest that these rocks were affected by burial metamorphism followed by an exhumation process during subduction tectonism in the BuC.展开更多
文摘Chickpea(Cicer arietinum L.) and pigeonpea [Cajanus cajan L.(Millsp.)] play an important role in mitigating protein malnutrition for millions of poor vegetarians living in regions of the semi-arid tropics. Abiotic stresses such as excess and limited soil moisture(water-logging and drought), heat and chilling(high and low temperature stresses), soil salinity, and acidity are major yield constraints, as these two crops are grown mostly under rainfed conditions in risk-prone marginal and degraded lands with few or no inputs. Losses due to such stresses vary from 30% to 100% depending on their severity. The literature abounds in basic information concerning screening techniques, physiological mechanisms, and genetics of traits associated with resistance/tolerance to abiotic stresses in these two crops. However, the final outcome in terms of resistant/tolerant varieties has been far from satisfactory. This situation calls for improving selection efficiency through precise phenotyping and genotyping under high-throughput controlled conditions using modern tools of genomics. In this review, we suggest that an integrated approach combining advances from genetics, physiology, and biotechnology needs to be used for higher precision and efficiency of breeding programs aimed at improving abiotic stress tolerance in both chickpea and pigeonpea.
文摘The amphibolites from the Mauranipur and Babina regions are located in the central part of the Bundelkhand Craton(BuC),northern India.During the geodynamic evolution of the BuC,these amphibolites underwent medium-grade metamorphism.This study combines textural observations of amphibolites from two distinct regions(Mauranipur and Babina)with mineral chemistry and phase equilibrium modelling.Observations suggest that the amphibolites of both areas have gone through three stages of metamorphism.The pre-peak stage in the amphibolites from the Mauranipur and Babina regions is marked by the assemblages Ep-Amp-Cpx-Pl-Ilm-Ru-Qz and Ep-Amp-Cpx-Pl-Ab-Ilm-Qz respectively;the peak metamorphic stage is characterized by the mineral assemblages Amp-Cpx-Pl-Ilm-Ru-Qz and Amp-Cpx-Pl-Ilm-Qz-H_(2)O,which is formed during the burial process,and the post-peak stage is represented by the assemblages Amp-Pl-Ilm-Ru-Qz and Amp-Pl-Ilm-Qz-H_(2)O respectively,which is formed by exhumation event.By applying the phase equilibria modelling in the NCFMASHTO system,the P-T conditions estimated from pre-peak,peak to post-peak stages are characterized as 6.7 kbar/510 oC,7.3 kbar/578ºC and>3.0 kbar/>585ºC,respectively,for the Mauranipur amphibolites;and 6.27 kbar/520ºC,5.2 kbar/805ºC and>3.0 kbar/>640ºC respectively for Babina amphibolites.The textural association and P-T conditions of both amphibolites suggest that these rocks were affected by burial metamorphism followed by an exhumation process during subduction tectonism in the BuC.
