Infection of radiata and bishop pine by Mycosphaerella pini in California

2005 ◽  
Vol 35 (11) ◽  
pp. 2529-2538 ◽  
Author(s):  
John A Muir ◽  
Fields W Cobb, Jr.

Infection of radiata pine (Pinus radiata D. Don) and bishop pine (Pinus muricata D. Don) by Myco sphaerella pini Rostr. in Munk was determined on needles of infected forest trees in central to northern coastal California. Conidia from infected trees were used to inoculate radiata pine seedlings maintained in constant and (or) fluctuating moisture and temperature regimes. On needles of radiata pine but not bishop pine plantation trees, most conidial germ tubes grew directly towards and entered the nearest epistomatal opening. On inoculated radiata pine seedlings in infection chambers, germ tubes grew haphazardly and few entered openings. Germ tubes entered epistomatal openings more often on abaxial than adaxial needle surfaces of both plantation trees and inoculated seedlings, and more lesions developed on the abaxial surface. Simple hyphae penetrated through epistomatal chambers, between guard cells, and into substomatal chambers. On radiata pine plantation trees, germ tubes that penetrated below guard cells occasionally formed substomatal vesicles. On needles of northern race bishop pine that had few disease lesions per needle, substomatal vesicles were common and frequently partially disintegrated. On seedlings, "water-soaked" spots formed 5 days after hyphae of the fungus penetrated slightly below guard cells. Development of typical lesions was delayed when seedlings were initially exposed to up to 16 days of continuous mist spray and then kept dry for 8 weeks. Penetration on inoculated seedlings was significantly greater in a variable than in a constant air temperature regime on abaxial needle surfaces, and greater in 24 h/day than in a 16 h/day exposure of seedlings to mist spray. In both temperature regimes more needles were infected on seedlings exposed to 24 h/day mist spray and fewest were infected in the variable temperature, 16 h/day moisture regime.

1983 ◽  
Vol 23 (121) ◽  
pp. 208 ◽  
Author(s):  
DW Flinn ◽  
RJ Waugh

A randomized block experiment was carried out in a radiata pine nursery at Benalla where the soil is weakly aggregated and slakes severely on wetting. Sunflower hulls or sudax ST6 hay or gypsum/dolomite were added during one cycle of a summer green crop, winter cover crop and a pine crop. Plots were also split for a deep ripping treatment. The aim was to improve soil conditions for the growth of pine seedlings. The addition of 170 t/ha of sunflower hulls reduced bulk density (P<0.01) and surface crust resistance (P< 0.05) and markedly increased infiltration capacity (P<0.01). Water-stable aggregation was not statistically affected by any of the treatments because the soil has a clay content of only 18%, though there was an encouraging trend of more water-stable aggregates within the size range 0.25-2 mm following the application of sunflower hulls. Germination of the pine crop was unaffected by treatments as the seed was covered with coarse sand. Seedling survival was low (range 41.1 -47.6%), due in part to saline conditions following fertilizer application. Early growth of seedlings was greater (P<0.05) where additional organic matter was incorporated, but differences between treatments were not statistically significant at harvest. We conclude that soil conditions can be improved for pine growth by adding a large quantity of organic matter, reducing cultivation and maintaining an intensive green cropping program.


Author(s):  
Eddy De Pauw

The countries of North Africa and West Asia, hereafter referred to as the “Near East,” cover a large part of the world (more than 7,200,000 km2). This region is characterized by diverse but generally dry climates, in which evaporation exceeds precipitation. The level of aridity is indicated by the aridity index, the ratio of annual precipitation to annual potential evapotranspiration, calculated by the Penman method (UNESCO, 1979). The degree of aridity is shown spatially in figure 16.1 and summarized per country in table 16.1. These data show that the region is characterized by humid, subhumid, semiarid, and arid to hyperarid moisture regimes. In addition, temperature regimes vary considerably, particularly due to the differences in altitudes and, to a lesser extent, due to the oceanic/continental influences. For most of the region, the precipitation generally occurs during the October–April period and thus is concentrated over the winter season. Table 16.1 shows that, with more than 90% of the land area in hyperarid, arid, or semiarid moisture regimes, aridity is very significant in the Near East. Turkey is better endowed with surface and groundwater resources due to the orographic capture of Atlantic cyclonal precipitation, but much of the interior is semiarid. If one excludes the hyperarid zones, which cover the driest deserts and have no potential for agricultural use, nearly 34% of the region, or about 2,460,000 km2, is dryland (i.e., the area with arid or semiarid moisture regime). These are the areas with some potential for either dryland farming (in semiarid zones) or for extensive rangeland (in arid zones). In the Near East countries, agriculture contributes about 10–20% to the gross domestic product and is therefore a major pillar of their economies. However, the indirect importance of agriculture is larger because it provides the primary goods that constitute the majority of merchandise exports and because of the relatively high number of people employed in agriculture. Because of the high degree of aridity in large parts of the region, agriculture in the Near East is particularly vulnerable to drought. Most of the agricultural systems depend on rainfall.


2020 ◽  
Vol 8 (8) ◽  
pp. 1171
Author(s):  
Anderson B. Mayfield

Unlike most parts of the world, coral reefs of Taiwan’s deep south have generally been spared from climate change-induced degradation. This has been linked to the oceanographically unique nature of Nanwan Bay, where intense upwelling occurs. Specifically, large-amplitude internal waves cause shifts in temperature of 6–9 °C over the course of several hours, and the resident corals not only thrive under such conditions, but they have also been shown to withstand multi-month laboratory incubations at experimentally elevated temperatures. To gain insight into the sub-cellular basis of acclimation to upwelling, proteins isolated from reef corals (Seriatopora hystrix) featured in laboratory-based reciprocal transplant studies in which corals from upwelling and non-upwelling control reefs (<20 km away) were exposed to stable or variable temperature regimes were analyzed via label-based proteomics (iTRAQ). Corals exposed to their “native” temperature conditions for seven days (1) demonstrated highest growth rates and (2) were most distinct from one another with respect to their protein signatures. The latter observation was driven by the fact that two Symbiodiniaceae lipid trafficking proteins, sec1a and sec34, were marginally up-regulated in corals exposed to their native temperature conditions. Alongside the marked degree of proteomic “site fidelity” documented, this dataset sheds light on the molecular mechanisms underlying acclimatization to thermodynamically extreme conditions in situ.


1967 ◽  
Vol 31 (3) ◽  
pp. 211-220 ◽  
Author(s):  
E. P. BACHELARD ◽  
VALERIE H. BOUGHTON
Keyword(s):  

Soil Research ◽  
2004 ◽  
Vol 42 (2) ◽  
pp. 189 ◽  
Author(s):  
C. R. Chen ◽  
L. M. Condron ◽  
B. L. Turner ◽  
N. Mahieu ◽  
M. R. Davis ◽  
...  

The effects of radiata pine (Pinus radiata D. Don) seedlings and ryegrass (Lolium perenne L.) on the mineralisation of orthophosphate monoesters in 7 grassland soils were assessed in a 10-month pot trial using NaOH–EDTA extraction and solution 31P NMR spectroscopy. Extraction with NaOH–EDTA recovered 46–86% of the total soil P, and NaOH–EDTA-extractable organic P determined by molybdate colourimetry ranged between 194 and 715 mg/kg soil, representing 34–85% of the total soil organic P. Orthophosphate monoesters were the predominant species of the extracted organic P in all soils, with much smaller concentrations of orthophosphate diesters, and traces of phosphonates. Concentrations of orthophosphate monoesters were consistently lower in soils under pine (103–480 mg P/kg soil) compared with the initial soils (142–598 mg P/kg soil) and most soils under grass (122–679 mg/kg soil). Mineralisation of myo-inositol hexakisphosphate accounted for 18–100% of the total mineralisation of orthophosphate monoesters in most soils under radiata pine. This suggests that supposedly recalcitrant inositol phosphates are available for uptake by radiata pine, although the extent of this varies among soils.


1986 ◽  
Vol 14 (2) ◽  
pp. 113-124 ◽  
Author(s):  
Ruth L. Gadgil ◽  
J.F.L. Charlton ◽  
Adriana M. Sandberg ◽  
P.J. Allen

1975 ◽  
Vol 107 (11) ◽  
pp. 1167-1174 ◽  
Author(s):  
R. E. Stinner ◽  
G. D. Butler ◽  
J. S. Bacheler ◽  
C. Tuttle

AbstractThe simulation of variability in temperature-dependent development is discussed. An algorithm for simulation of this variability is developed and validated under constant and variable temperature regimes for Anthonomus grandis, Trichoplusia ni, and Heliothis zea.


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