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			<titleStmt><title level='a'>Stepping forward from relevance in mycorrhizal ecology</title></titleStmt>
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				<publisher></publisher>
				<date>04/01/2020</date>
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				<bibl> 
					<idno type="par_id">10191210</idno>
					<idno type="doi">10.1111/nph.16432</idno>
					<title level='j'>New Phytologist</title>
<idno>0028-646X</idno>
<biblScope unit="volume">226</biblScope>
<biblScope unit="issue">2</biblScope>					

					<author>Gabriel R. Smith</author><author>Kabir G. Peay</author>
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			<abstract><ab><![CDATA[]]></ab></abstract>
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<div xmlns="http://www.tei-c.org/ns/1.0"><p>Over the past decade, categorizing plants by the mycorrhizal fungi on their roots has allowed us to collapse the complexity of plant life's hidden, belowground half into a simple, sometimes even binary variable. Most plants are now being classified as associating primarily with ectomycorrhizal or arbuscular mycorrhizal fungi to facilitate soil nutrient uptake <ref type="bibr">(Brundrett &amp; Tedersoo, 2018</ref>; but see <ref type="bibr">Bueno et al., 2019)</ref>. A plant's mycorrhizal 'type' predicts its soil environment's carbon (C) and nitrogen (N) stocks <ref type="bibr">(Averill et al., 2014;</ref><ref type="bibr">Cotrufo et al., 2019)</ref>, its response to global change pressures <ref type="bibr">(Terrer et al., 2016;</ref><ref type="bibr">Averill et al., 2018)</ref>, and even its global biogeography <ref type="bibr">(Steidinger et al., 2019)</ref>. Mycorrhizal fungi are no longer journeying towards relevance to broader ecosystem science and biogeochemistry, as once suggested <ref type="bibr">(Read &amp; Perez-Moreno, 2003)</ref> they have arrived.</p><p>'. . . the coming era of mycorrhizal ecology and its path forward from relevance ought to be built not upon plant and fungal binaries, but upon continua and communities.'</p><p>Biogeochemical differences between ectomycorrhizal-and arbuscular mycorrhizal-associated plants and ecosystems, for example that the former have higher soil C : N ratios <ref type="bibr">(Averill et al., 2014)</ref> and a stronger carbon dioxide (CO 2 ) fertilization response <ref type="bibr">(Terrer et al., 2016)</ref> than the latter, are often attributed to physiological differences between ectomycorrhizal and arbuscular mycorrhizal fungi. Indeed, ectomycorrhizal fungi generally take up organic nutrients from soil more effectively than arbuscular mycorrhizal fungi do, which can affect whole-ecosystem elemental cycling <ref type="bibr">(Orwin et al., 2011;</ref><ref type="bibr">Phillips et al., 2013)</ref>. But if trait differences between ectomycorrhizal and arbuscular mycorrhizal plants and fungi can cause ecosystem function to diverge, then the scale at which meaningful variation occurs, whether between or within groups, could affect the scale at which such patterns emerge. A reasonable simplification has brought us relevance, but refinement thereof might thus offer even greater utility.</p><p>In this issue of New Phytologist, <ref type="bibr">Fernandez et al. (2020;</ref><ref type="bibr">pp. 569-582)</ref> invite us to expand our thinking. The Gadgil effect, where resource uptake, especially of organic N, by ectomycorrhizal fungi slows litter decomposition by starving free-living saprotrophs <ref type="bibr">(Fernandez &amp; Kennedy, 2016)</ref>, is hypothesized to drive soil C accumulation in ectomycorrhizal ecosystems <ref type="bibr">(Orwin et al., 2011;</ref><ref type="bibr">Averill et al., 2014)</ref>. However, theory predicts its occurrence only where ectomycorrhizal N mining abilities are strong and litter N is hard to access <ref type="bibr">(Smith &amp; Wan, 2019)</ref>. Testing this prediction, Fernandez et al. performed a reciprocal litter decomposition and mycorrhizal exclusion experiment in two ectomycorrhizal forests, each with different leaf litter chemistry and a different ectomycorrhizal fungal community.</p><p>Excluding roots and mycorrhizal fungi in a pine forest accelerated the decomposition of pine litter but not of oak litter, while the same treatment in an oak forest had no effect on the decomposition of either litter. Only where recalcitrant litter and an ectomycorrhizal community adapted to it co-occurred could ectomycorrhizal N uptake slow decomposition. Fernandez et al. thus show that the same divergence in ecosystem function we expect to see across plant communities of different mycorrhizal type can also be found where mycorrhizal type does not differ, because the traits of the resident plants and fungi may nevertheless vary. In doing so, they demonstrate that the coming era of mycorrhizal ecology and its path forward from relevance ought to be built not upon plant and fungal binaries, but upon continua and communities.</p><p>In addition to expanding our basic knowledge about mycorrhizal functioning, these findings also allow us to take a step towards more detailed spatial predictions of ectomycorrhizal effects on nutrient cycling. To illustrate this point visually, we combined forest inventory data from the US Forest Service, tree leaf litter trait measurements drawn from the literature, and occurrence records of Tomentella, the dominant ectomycorrhizal genus in the pine forest studied by <ref type="bibr">Fernandez et al., from the Global Biodiversity Information Facility (GBIF.org, 2019)</ref>. Then, we generated a map of the contiguous United States depicting the average litter lignin : N ratio of measured forest plots, their primary mycorrhizal type, and the locations where Tomentella has been reported (Fig. <ref type="figure">1</ref>).</p><p>Based on the results of Fernandez et al., we speculate that the Gadgil effect should be most pronounced in ectomycorrhizal forests with high litter lignin : N ratios where Tomentella is common. In Fig. <ref type="figure">1</ref>, regional gradients of litter lignin : N ratio appear nested within larger, continent-wide gradients, indicating that the strength of the Gadgil effect probably varies at multiple scales. Though Tomentella is widely distributed, ectomycorrhizal fungal community turnover, which also occurs at scales spanning several orders of magnitude <ref type="bibr">(Smith et al., 2018)</ref>, is another likely source of variation. This suggests that coordinated, hierarchically structured research efforts, perhaps similar in design to prior studies of litter decomposition (e.g. <ref type="bibr">Bradford et al., 2017)</ref>, could be useful for determining the relative contributions of aboveground and belowground trait variation to ecosystem biogeochemistry. Additionally, since it is not clear which specific traits enable Tomentella</p><p>This article is a Commentary on Fernandez et al., 226: 569-582. 292 New Phytologist (2020) 226: 292-294 &#211; 2020 The Authors New Phytologist &#211; 2020 New Phytologist Trust <ref type="url">www.newphytologist.com</ref> </p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head>Forum</head><p>to compete effectively with saprotrophs, such projects could benefit from the application and development of trait databases like Fun Fun <ref type="bibr">(Zanne et al., 2019)</ref> to identify other important, functionally analogous taxa.</p><p>Our field's progress over the past 10 years has been remarkable, and we may be rightfully pleased with our achievements. The coming decade of mycorrhizal research will surely bring more fascinating discoveries, some lending support to long-held hypotheses and others defying our wildest expectations. However, the findings of Fernandez et al. demonstrate that answering the many remaining questions in mycorrhizal ecology will best be served by approaching them with an open mind rather than restricting our thinking to the same conceptual frameworks that have brought us here. Together, we have reached a notable height. As has long been emphasized <ref type="bibr">(Wumen, 1228)</ref>, we are confident that the greatest benefit will now be gained not by clinging to our perch or admiring the view, but by stepping forward.</p></div>			<note xmlns="http://www.tei-c.org/ns/1.0" place="foot" n="1" xml:id="foot_0"><p>Department of Biology, Stanford University, 371 Jane Stanford Way, Stanford, CA 94305, USA;</p></note>
			<note xmlns="http://www.tei-c.org/ns/1.0" place="foot" n="2" xml:id="foot_1"><p>Global Ecosystem Ecology, Department of Environmental Systems Science, Institute of Integrative Biology, ETH Z&#8364; urich, 8092 Z&#8364; urich, Switzerland (*Author for correspondence: tel +1 650 736 6676; email grsmith@stanford.edu)</p></note>
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