Poplar and shrub willow energy crops in the United States: field trial results from the multiyear regional feedstock partnership and yield potential maps based on the PRISM‐ELM model

To increase the understanding of poplar and willow perennial woody crops and facilitate their deployment for the production of biofuels, bioproducts, and bioenergy, there is a need for broadscale yield maps. For national analysis of woody and herbaceous crops production potential, biomass feedstock yield maps should be developed using a common framework. This study developed willow and poplar potential yield maps by combining data from a network of willow and poplar field trials and the modeling power of PRISM‐ELM. Yields of the top three willow cultivars across 17 sites ranged from 3.60 to 14.6 Mg ha^?1 yr^?1 dry weight, while the yields from 17 poplar trials ranged from 7.5 to 15.2 Mg ha^?1 yr^?1. Relationships between the environmental suitability estimates from the PRISM‐ELM model and results from field trials had an R² of 0.60 for poplar and 0.81 for willow. The resulting potential yield maps reflected the range of poplar and willow yields that have been reported in the literature. Poplar covered a larger geographic range than willow, which likely reflects the poplar breeding efforts that have occurred for many more decades using genotypes from a broader range of environments than willow. While the field trial data sets used to develop these models represent the most complete information at the time, there is a need to expand and improve the model by monitoring trials over multiple cutting cycles and across a broader range of environmental gradients. Despite some limitations, the results of these models represent a dramatic improvement in projections of potential yield of poplar and willow crops across the United States.     

Dynamics of Human Replication Protein A Subunit Distribution and Partitioning in the Cell Cycle

Human replication protein A (RPA) is a three-subunit protein complex involved in DNA replication, repair, and recombination. To gain insight into the dynamics of subunit assembly, we examined the subcellular distribution of RPA subunits (p70, p34, and p11) during the cell cycle. All three subunits colocalized in G1 and S phases, showing a diffuse nuclear distribution in G1 but a dot-like nuclear pattern in S phase. During S phase, the subunits showed a pattern reminiscent of the replication granules/factories described by others as sites of replication machinery. In metaphase, p70 preferentially associated with the spindle poles, p34 was found on chromosomes, and p11 remained in the cytoplasm. In telophase, p70 and p34 appeared in the forming daughter nuclei; p11 remained in the cytoplasm until G1. Among the three subunits only p34 was associated with the nuclear matrix and this association persisted throughout the cell cycle. We conclude that (i) RPA complex assembly is differentially regulated, (ii) the replication machinery may be anchored to the nuclear matrix, and (iii) RPA subunits partition during mitosis and sort into daughter nuclei by different routes.     

Carbon fluxes in the rhizosphere of sweet chestnut seedlings (Castanea sativa) grown under two atmospheric CO2 concentrations: 14C partitioning after pulse labelling

Partitioning of ¹⁴C was assessed in sweet chestnut seedlings (Castanea sativa Mill.) grown in ambient and elevated atmospheric [CO₂] environments during two vegetative cycles. The seedlings were exposed to ¹⁴CO₂ atmosphere in both high and low [CO₂] environments for a 6-day pulse period under controlled laboratory conditions. Six days after exposure to ¹⁴CO₂, the plants were harvested, their dry mass and the radioactivity were evaluated. ¹⁴C concentration in plant tissues, root-soil system respiratory outputs and soil residues (rhizodeposition) were measured. Root production and rhizodeposition were increased in plants growing in elevated atmospheric [CO₂]. When measuring total respiration, i.e. CO₂ released from the root/soil system, it is difficult to separate CO₂ originating from roots and that coming from the rhizospheric microflora. For this reason a model accounting for kinetics of exudate mineralization was used to estimate respiration of rhizospheric microflora and roots separately. Root activity (respiration and exudation) was increased at the higher atmospheric CO₂ concentration. The proportion attributed to root respiration accounted for 70 to 90% of the total respiration. Microbial respiration was related to the amount of organic carbon available in the rhizosphere and showed a seasonal variation dependent upon the balance of root exudation and respiration. The increased carbon assimilated by plants grown under elevated atmospheric [CO₂] stayed equally distributed between these increased root activities. ei]H Lambers     

Delocalization over the heme and the axial ligands of one of the two oxidizing equivalents stored above the ferric state in the peroxidase and catalase Compound-I intermediates: indirect participation of the proximal axial ligand of iron in the oxidation reactions catalyzed by heme-based peroxidases and catalases?

 A comparison of the exchange interactions arising in the peroxidase and catalase Compound I intermediates and their iron(IV)-oxo porphyrin π-cation radical models, both of which are two oxidizing equivalents above the ferric state, suggests that in the models the oxidizing equivalent is localized on the porphyrin ring, while in the proteins it is partly delocalized onto the proximal ligand. Thus, the proximal axial ligand of iron participates indirectly in the oxidation reactions catalyzed by the enzymes. Possible roles of the axial ligand in the catalytic mechanism of these heme-based enzymes are discussed. Received and accepted: 7 May 1996     

Phenoxyl-copper(II) complexes: models for the active site of galactose oxidase

 The reaction of the macrocycles 1,4,7-tris (3,5-di-tert-butyl-2-hydroxy-benzyl)-1,4,7-triazacyclononane, L¹H₃, or 1,4,7-tris(3-tert-butyl-5-methoxy-2-hydroxy-benzyl)-1,4,7-triazacyclononane, L²H₃, with Cu(ClO₄)₂·6H₂O in methanol (in the presence of Et₃N) affords the green complexes [Cu^II(L¹H)] (1), [Cu^II(L²H)]·CH₃OH (2) and (in the presence of HClO₄) [Cu^II(L¹H₂)](ClO₄) (3) and [Cu^II(L²H₂)] (ClO₄) (4). The Cu^II ions in these complexes are five-coordinate (square-base pyramidal), and each contains a dangling, uncoordinated pendent arm (phenol). Complexes 1 and 2 contain two equatorially coordinated phenolato ligands, whereas in 3 and 4 one of these is protonated, affording a coordinated phenol. Electrochemically, these complexes can be oxidized by one electron, generating the phenoxyl-copper(II) species [Cu^II(L¹H)]^+ ·, [Cu(L²H)]^+ ·, [Cu^II(L¹H₂)]^2+ ·, and [Cu^II(L²H₂)]^2+ ·, all of which are EPR-silent. These species are excellent models for the active form of the enzyme galactose oxidase (GO). Their spectroscopic features (UV-VIS, resonance Raman) are very similar to those reported for GO and unambiguously show that the complexes are phenoxyl-copper(II) rather than phenolato-copper(III) species. Received: 10 February 1997 / Accepted: 7 April 1997     

A scaling approach for quantifying the net CO2 flux of the Kuparuk River Basin,Alaska

Net CO₂ flux measurements conducted during the summer and winter of 1994–96 were scaled in space and time to provide estimates of net CO₂ exchange during the 1995–96 (9 May 1995–8 May 1996) annual cycle for the Kuparuk River Basin, a 9200 km² watershed located in NE Alaska. Net CO₂ flux was measured using dynamic chambers and eddy covariance in moist‐acidic, nonacidic, wet‐sedge, and shrub tundra, which comprise 95% of the terrestrial landscape of the Kuparuk Basin. CO₂ flux data were used as input to multivariate models that calculated instantaneous and daily rates of gross primary production (GPP) and whole‐ecosystem respiration (R) as a function of meteorology and ecosystem development. Net CO₂ flux was scaled up to the Kuparuk Basin using a geographical information system (GIS) consisting of a vegetation map, digital terrain map, dynamic temperature and radiation fields, and the models of GPP and R. Basin‐wide estimates of net CO₂ exchange for the summer growing season (9 May?5 September 1995) indicate that nonacidic tundra was a net sink of ?31.7 ± 21.3 GgC (1 Gg = 10⁹ g), while shrub tundra lost 32.5 ± 6.3 GgC to the atmosphere (negative values denote net ecosystem CO₂ uptake). Acidic and wet sedge tundra were in balance, and when integrated for the entire Kuparuk River Basin (including aquatic surfaces), whole basin summer net CO₂ exchange was estimated to be in balance (?0.9 ± 50.3 GgC). Autumn to winter (6 September 1995–8 May 1996) estimates of net CO₂ flux indicate that acidic, nonacidic, and shrub tundra landforms were all large sources of CO₂ to the atmosphere (75.5 ± 8.3, 96.4 ± 11.4, and 43.3 ± 4.7 GgC for acidic, nonacidic, and shrub tundra, respectively). CO₂ loss from wet sedge surfaces was not substantially different from zero, but the large losses from the other terrestrial landforms resulted in a whole basin net CO₂ loss of 217.2 ± 24.1 GgC during the 1995–96 cold season. When integrated for the 1995–96 annual cycle, acidic (66.4 + 25.25 GgC), nonacidic (64.7 ± 29.2 GgC), and shrub tundra (75.8 ± 8.4 GgC) were substantial net sources of CO₂ to the atmosphere, while wet sedge tundra was in balance (0.4 + 0.8 GgC). The Kuparuk River Basin as a whole was estimated to be a net CO₂ source of 218.1 ± 60.6 GgC over the 1995–96 annual cycle. Compared to direct measurements of regional net CO₂ flux obtained from aircraft‐based eddy covariance, the scaling procedure provided realistic estimates of CO₂ exchange during the summer growing season. Although winter estimates could not be assessed directly using aircraft measurements of net CO₂ exchange, the estimates reported here are comparable to measured values reported in the literature. Thus, we have high confidence in the summer estimates of net CO₂ exchange and reasonable confidence in the winter net CO₂ flux estimates for terrestrial landforms of the Kuparuk river basin. Although there is larger uncertainty in the aquatic estimates, the small surface area of aquatic surfaces in the Kuparuk river basin (≈ 5%) presumably reduces the potential for this uncertainty to result in large errors in basin‐wide CO₂ flux estimates.     

The iron-sulfur clusters in 2-hydroxyglutaryl-CoA dehydratase from Acidaminococcus fermentans. Biochemical and spectroscopic investigations.

The reversible dehydration of (R)-2-hydroxyglutaryl-CoA to (E)-glutaconyl-CoA is catalysed by the combined action of two oxygen-sensitive enzymes from Acidaminococcus fermentans, the homodimeric component A (2 x 27 kDa) and the heterodimeric component D (45 and 50 kDa). Component A was purified to homogeneity (specific activity 25-30 s-1) using streptavidin-tag affinity chromatography. In the presence of 5 mM MgCl2 and 1 mM ADP or ATP, component A could be stabilized and stored for 4-5 days at 4 degrees C without loss of activity. The purification of component D from A. fermentans was also improved as indicated by the 1.5-fold higher specific activity (15 s-1). The content of 1.0 riboflavin 5'-phosphate (FMN) per heterodimer could be confirmed, whereas in contrast to an earlier report only trace amounts of riboflavin (< 0.1) could be detected. Each active component contains an oxygen sensitive diamagnetic [4Fe-4S]2+ cluster as revealed by UV-visible, EPR and M?ssbauer spectroscopy. Reduction of the [4Fe-4S]2+ cluster in component A with dithionite yields a paramagnetic [4Fe-4S]1+ cluster with the unusual electron spin ground state S = 3/2 as indicated by strong absorption type EPR signals at high g values, g = 4-6. Spin-Hamiltonian simulations of the EPR spectra and of magnetic M?ssbauer spectra were performed to determine the zero field splitting (ZFS) parameters of the cluster and the 57Fe hyperfine interaction parameters. The electronic properties of the [4Fe-4S]2+, 1+ clusters of component A are similar to those of the nitrogenase iron protein in which a [4Fe-4S]2+ cluster bridges the two subunits of the homodimeric protein. Under air component A looses its activity within seconds due to irreversible degradation of its [4Fe-4S]2+ cluster to a [2Fe-2S]2+ cluster. The [4Fe-4S]2+ cluster of component D could not be reduced to a [4Fe-4S]1+ cluster, even with excess of Ti(III)citrate or dithionite. Exposure to oxic conditions slowly converts the diamagnetic [4Fe-4S]2+ cluster of component D to a paramagnetic [3Fe-4S]+ cluster concomitant with loss of activity (30% within 24 h at 4 degrees C).     

Hosts of Mediterranean fruit fly Ceratitis capitata (Wiedemann) (Diptera: Tephritidae) from Broome and the Broome Peninsula, Western Australia

Abstract  In the Kimberley region of Western Australia, Mediterranean fruit fly (medfly) Ceratitis capitata (Wiedemann) (Diptera: Tephritidae) is only established at Broome. From 1998 to 2001 extensive fruit sampling was carried out at Broome during a trial investigating the eradication of medfly from the Kimberley using the sterile insect technique. Fruit was collected from 82 native and introduced plants growing in and surrounding the town of Broome and held for emergence of medfly. Eighteen plants, including the native tree Terminalia petiolaris , were found to be medfly hosts . On the basis of abundance, fruiting phenology and host suitability, eight species (kumquat Fortunella japonica , mango Magnifera indica , Barbados cherry Malpighia glabra , orange jessamine Murraya paniculata , guava Psidium guajava , Pacific almond Terminalia catapa , blackberry tree Terminalia petiolaris and yellow oleander Thevetia peruviana ) were the most important hosts ensuring medfly survival and population growth. Despite medfly being reared from T. petiolaris , it is likely that medfly can only maintain populations in areas close to human habitation, and eradication from these areas would lead to eradication from the whole Kimberley region.