Author Correction: Climatic controls of decomposition drive the global biogeography of forest-tree symbioses.

In this Letter, a middle initial and additional affiliation have been added for author G. J. Nabuurs; two statements have been added to the Supplementary Acknowledgements; and a citation to the French National Institute has been added to the Methods; see accompanying Author Correction for further details.

Climatic controls of decomposition drive the global biogeography of forest-tree symbioses.

The identity of the dominant root-associated microbial symbionts in a forest determines the ability of trees to access limiting nutrients from atmospheric or soil pools1,2, sequester carbon3,4 and withstand the effects of climate change5,6. Characterizing the global distribution of these symbioses and identifying the factors that control this distribution are thus integral to understanding the present and future functioning of forest ecosystems. Here we generate a spatially explicit global map of the symbiotic status of forests, using a database of over 1.1 million forest inventory plots that collectively contain over 28,000 tree species. Our analyses indicate that climate variables-in particular, climatically controlled variation in the rate of decomposition-are the primary drivers of the global distribution of major symbioses. We estimate that ectomycorrhizal trees, which represent only 2% of all plant species7, constitute approximately 60% of tree stems on Earth. Ectomycorrhizal symbiosis dominates forests in which seasonally cold and dry climates inhibit decomposition, and is the predominant form of symbiosis at high latitudes and elevation. By contrast, arbuscular mycorrhizal trees dominate in aseasonal, warm tropical forests, and occur with ectomycorrhizal trees in temperate biomes in which seasonally warm-and-wet climates enhance decomposition. Continental transitions between forests dominated by ectomycorrhizal or arbuscular mycorrhizal trees occur relatively abruptly along climate-driven decomposition gradients; these transitions are probably caused by positive feedback effects between plants and microorganisms. Symbiotic nitrogen fixers-which are insensitive to climatic controls on decomposition (compared with mycorrhizal fungi)-are most abundant in arid biomes with alkaline soils and high maximum temperatures. The climatically driven global symbiosis gradient that we document provides a spatially explicit quantitative understanding of microbial symbioses at the global scale, and demonstrates the critical role of microbial mutualisms in shaping the distribution of plant species.

Solubilization of DMPC and DPPC vesicles by detergents below their critical micellization concentration: high-sensitivity differential scanning calorimetry, Fourier transform infrared spectroscopy and freeze-fracture electron microscopy reveal two interaction sites of detergents in vesicles.

The interaction of sodium deoxycholate, sodium cholate and octyl glucoside with sonicated vesicles of L alpha-dimyristoyl-phosphatidylcholine (DMPC) and L alpha-dipalmitoylphosphatidylcholine (DPPC) at concentrations below the critical micellization concentration (cmc) of the detergents was studied by high-sensitivity DSC (hs-DSC), Fourier transform infrared spectroscopy (FT-IR) and freeze-fracture electron microscopy. The two phospholipids exhibited a striking different thermotropic behaviour in the presence of these detergents. For DPPC vesicles, the detergents were found to interact exclusively in the aqueous interface region of the bilayer below the membrane saturation concentration Rsat while in DMPC vesicles two coexisting interaction sites below this concentration persist. These are detergents which interact at the aqueous interface region (site 1) and in the acyl chain region (site 2) of the DMPC vesicles. The partition coefficients K of the detergents between DPPC vesicles and the water phase were calculated from the hs-DSC results at two detergent/phospholipid molar ratios Rtot less than or equal to Rsat as 0.35, 0.049 and 0.040 mol-1 for sodium deoxycholate, sodium cholate and octyl glucoside, respectively. In contrast, for DMPC the K values for Rtot less than or equal to Rsat were found to be dependent on Rtot due to the occupation of site 2 by the detergents above a certain Rtot. The model is discussed on the basis of the detergents free energies of transfer from the water phase to site 1 and site 2 of the vesicles, respectively. The solubilization behaviour of DPPC vesicles, dependent on whether the total detergent concentration is above or below the cmc at Rsat, differed significantly as revealed by hs-DSC. This suggests that in the latter case an additional hydrophobic effect could facilitate the formation of disc shaped mixed micelles. Moreover, this different behaviour was employed to measure the cmc values of the detergents studied in the presence of the vesicles by hs-DSC.

Relationship between bronchial response to respiratory heat exchange and nonspecific airways reactivity in asthmatic patients.

In this study we have examined the relationship between the bronchial response to inhaled histamine and the bronchial response to breathing cold air at rest in nine control subjects and nine patients with asthma. Dried warm air (mean temp: +/- 1SD: 25.4 +/- 1.6 degrees C) and cold air (-19.7 +/- 2.6 degrees C) were breathed for 10 minutes each during quiet breathing at rest prior to as well as during both measurements of forced expired spirograms and the phase 3 slope of the single-breath oxygen test (delta N2/L). Subjects were also challenged with inhaled aerosolized histamine to determine the concentration required to reduce the forced expired volume in one second (FEV1) by 20 percent (PC20). Both asthmatic and control subjects had significantly greater respiratory heat exchange breathing cold as compared to warm air (p less than 0.01 in both cases). Control subjects did not change FEV1 or delta N2/L breathing cold air. Asthmatic patients increased delta N2/L from a mean warm air value of 2.41 +/- 1.31% N2/L to a mean cold air value of 5.39 +/- 4.55% N2/L (p less than 0.05). There was a significant linear correlation between the percent increase in delta N2/L from warm to cold air and 1/log10PC20 (r = -0.97, p less than 0.001) and also the percent decrease in FEV1 and log PC20 (r = -0.76, p less than 0.03) in the asthmatic patients. We conclude that cold air-induced alterations in ventilation/distribution and expired flow rates in asthmatic patients are related to pre-existing nonspecific airways reactivity.

Recurrent nocturnal asthma after bronchoprovocation with Western Red Cedar sawdust: association with acute increase in non-allergic bronchial responsiveness.

Recurrent nocturnal asthma following a single exposure to Western Red Cedar sawdust was documented by measurements of peak flow rates in two sensitized subjects. The nocturnal asthma followed a dual asthmatic response in the first subject and a late (non-immediate) asthmatic response in the second. Both subjects developed a 10-fold reduction in the dose of histamine required to decrease the FEV1 by 20%. This cedar-induced increase in non-specific bronchial reactivity was maximal at the time of the recurrent nocturnal asthma, and persisted after nocturnal asthma had ceased and after FEV1 had returned to normal. We hypothesize that the enhanced non-specific bronchial reactivity which occurs following late asthmatic responses to bronchial challenge is the cause of recurrent nocturnal asthma following single exposure to a sensitizing agent.