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        <title>Nova Reader - Subject</title>
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        <copyright>Newgen KnowledgeWorks</copyright>
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            <title><![CDATA[Topsoil organic matter build‐up in glacier forelands around the world]]></title>
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            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15496</link>
            <description><![CDATA[<p class="para" id="N65542">Since the last glacial maximum, soil formation related to ice‐cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that control carbon and nitrogen sequestration rates and biogeochemical stability of newly sequestered carbon, remain poorly understood. Here, we investigate the build‐up of SOM during the initial stages (up to 410 years) of topsoil development in 10 glacier forelands distributed on four continents. We test whether the net accumulation of SOM on glacier forelands (i) depends on the time since deglacierization and local climatic conditions (temperature and precipitation); (ii) is accompanied by a decrease in its stability and (iii) is mostly due to an increasing contribution of organic matter from plant origin. We measured total SOM concentration (carbon, nitrogen), its relative hydrogen/oxygen enrichment, stable isotopic (<sup>13</sup>C, <sup>15</sup>N) and carbon functional groups (C‐H, C=O, C=C) compositions, and its distribution in carbon pools of different thermal stability. We show that SOM content increases with time and is faster on forelands experiencing warmer climates. The build‐up of SOM pools shows consistent trends across the studied soil chronosequences. During the first decades of soil development, the low amount of SOM is dominated by a thermally stable carbon pool with a small and highly thermolabile pool. The stability of SOM decreases with soil age at all sites, indicating that SOM storage is dominated by the accumulation of labile SOM during the first centuries of soil development, and suggesting plant carbon inputs to soil (SOM depleted in nitrogen, enriched in hydrogen and in aromatic carbon). Our findings highlight the potential vulnerability of SOM stocks from proglacial areas to decomposition and suggest that their durability largely depends on the relative contribution of carbon inputs from plants.</p><p class="para" id="N65541">In glacier forelands all over the world, the organic matter build‐up during the initial stages of topsoil development is strongly modulated by climate: a warmer climate accelerates accumulation of organic matter. We also detected a decreasing thermal stability of soil organic matter along the chronosequences. The observed changes in soil organic matter elemental stoichiometry, aromaticity and stable isotope signature with soil organic matter accumulation suggest an increasing contribution of organic matter from plant origin during the first centuries of topsoil development.
<div class="section"><div class="box" id="N65543"><div class="imageVideo"><img src="/dataresources/secured/content-1766033099687-45bc64e2-42d2-4f7c-8c4a-1c43a08b5ad7/assets/GCB-27-1662-g006.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2021-01-16T00:00]]></pubDate>
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            <title><![CDATA[Heatwave‐induced synchrony within forage fish portfolio disrupts energy flow to top pelagic predators]]></title>
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            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15556</link>
            <description><![CDATA[<p class="para" id="N65542">During the Pacific marine heatwave of 2014–2016, abundance and quality of several key forage fish species in the Gulf of Alaska were simultaneously reduced throughout the system. Capelin (<i>Mallotus catervarius</i>), sand lance (<i>Ammodytes personatus</i>), and herring (<i>Clupea pallasii</i>) populations were at historically low levels, and within this community abrupt declines in portfolio effects identify trophic instability at the onset of the heatwave. Although compensatory changes in age structure, size, growth or energy content of forage fish were observed to varying degrees among all these forage fish, none were able to fully mitigate adverse impacts of the heatwave, which likely included both top‐down and bottom‐up forcing. Notably, changes to the demographic structure of forage fish suggested size‐selective removals typical of top‐down regulation. At the same time, changes in zooplankton communities may have driven bottom‐up regulation as copepod community structure shifted toward smaller, warm water species, and euphausiid biomass was reduced owing to the loss of cold‐water species. Mediated by these impacts on the forage fish community, an unprecedented disruption of the normal pelagic food web was signaled by higher trophic level disruptions during 2015–2016, when seabirds, marine mammals, and groundfish experienced shifts in distribution, mass mortalities, and reproductive failures. Unlike decadal‐scale variability underlying ecosystem regime shifts, the heatwave appeared to temporarily overwhelm the ability of the forage fish community to buffer against changes imposed by warm water anomalies, thereby eliminating any ecological advantages that may have accrued from having a suite of coexisting forage species with differing life‐history compensations.</p><p class="para" id="N65541">The Pacific marine heatwave was a prolonged warming event that led to reduced abundance and quality of small pelagic forage fishes. This caused a major disruption in the pelagic marine food web that precipitated large‐scale mortality and reproductive failures in upper trophic level predators. Unlike decadal‐scale variability underlying ecosystem regime shifts, the heatwave appeared to temporarily overwhelm the ability of the middle trophic level to buffer against changes imposed by warm water anomalies.<div class="section"><div class="box" id="N65543"><div class="imageVideo"><img src="/dataresources/secured/content-1766030219109-642d019f-20c6-4b9a-9403-441b5f8dd12e/assets/GCB-27-1859-g002.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2021-03-06T00:00]]></pubDate>
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            <title><![CDATA[Leaching of dissolved organic carbon from mineral soils plays a significant role in the terrestrial carbon balance]]></title>
            <media:thumbnail url="https://storage.googleapis.com/nova-demo-unsecured-files/unsecured/content-1765948350992-ac369ee2-628d-40e4-9a38-76659f8b6d66/cover.png"></media:thumbnail>
            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15460</link>
            <description><![CDATA[<p class="para" id="N65542">The leaching of dissolved organic carbon (DOC) from soils to the river network is an overlooked component of the terrestrial soil C budget. Measurements of DOC concentrations in soil, runoff and drainage are scarce and their spatial distribution highly skewed towards industrialized countries. The contribution of terrestrial DOC leaching to the global‐scale C balance of terrestrial ecosystems thus remains poorly constrained. Here, using a process based, integrative, modelling approach to upscale from existing observations, we estimate a global terrestrial DOC leaching flux of 0.28 ± 0.07 Gt C year<sup>−1</sup> which is conservative, as it only includes the contribution of mineral soils. Our results suggest that globally about 15% of the terrestrial Net Ecosystem Productivity (NEP, calculated as the difference between Net Primary Production and soil respiration) is exported to aquatic systems as leached DOC. In the tropical rainforest, the leached fraction of terrestrial NEP even reaches 22%. Furthermore, we simulated spatial‐temporal trends in DOC leaching from soil to the river networks from 1860 to 2010. We estimated a global increase in terrestrial DOC inputs to river network of 35 Tg C year<sup>−1</sup> (14%) from 1860 to 2010. Despite their low global contribution to the DOC leaching flux, boreal regions have the highest relative increase (28%) while tropics have the lowest relative increase (9%) over the historical period (1860s compared to 2000s). The results from our observationally constrained model approach demonstrate that DOC leaching is a significant flux in the terrestrial C budget at regional and global scales.</p><p class="para" id="N65541">Using a process‐based, integrative, modelling approach to upscale from existing observations, we estimate a global terrestrial DOC leaching flux of 0.28 ± 0.07 Gt C year<sup>−1</sup> which is conservative, as it only includes the contribution of mineral soils. Our results suggest that globally about 15% of the terrestrial Net Ecosystem Productivity is exported to aquatic systems as leached DOC. In the tropical rainforest, the leached fraction of terrestrial NEP even reaches 22%.<div class="section"><div class="box" id="N65546"><div class="imageVideo"><img src="/dataresources/secured/content-1765948350992-ac369ee2-628d-40e4-9a38-76659f8b6d66/assets/GCB-27-1083-g010.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-12-14T00:00]]></pubDate>
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            <title><![CDATA[Inhibitory effects of climate change on the growth and extracellular enzyme activities of a widespread Antarctic soil fungus]]></title>
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            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15456</link>
            <description><![CDATA[<p class="para" id="N65542">Temperatures approaching or exceeding 20°C have been measured during summer in polar regions at the surfaces of barren fellfield soils under cloudless skies around solar noon. However, despite the upper temperature limit for the growth of cold‐adapted microbes—which are abundant in polar soils and have pivotal roles in nutrient cycling—typically being close to this temperature, previous studies have not addressed the consequences of climate change for the metabolism of these organisms in the natural environment. Here in a 5‐year field experiment on Alexander Island in the southern maritime Antarctic, we show that the abundance of <i>Pseudogymnoascus roseus</i>, the most widespread decomposer fungus in maritime Antarctic fellfield soils, is reduced by 1–2 orders of magnitude when irrigated and nutrient‐amended soils are warmed to &gt;20°C during summer. Laboratory experiments under conditions mimicking those during midsummer in the natural environment indicated that the hyphal extension rates of <i>P. roseus</i> isolates and the activities of five extracellular enzymes are reduced by 54%–96% at high water availability after exposure to temperatures cycling daily from 2 to 21°C and 2 to 24°C, relative to temperatures cycling from 2 to 18°C. Given that the temperatures of surface soils at the study site already reach 19°C during midsummer, the observations reported here suggest that, at predicted rates of warming arising from moderate greenhouse gas emissions, inhibitory effects of climate change on the metabolism of <i>P. roseus</i> could manifest themselves within the next few decades. Furthermore, with peak temperatures at the surfaces of fellfield soils at other maritime Antarctic locations and in High Arctic and alpine regions already exceeding 20°C during summer, the observations suggest that climate warming has the potential to inhibit the growth of other cold‐adapted microbes, with negative effects on soils as the Earth's climate continues to warm.</p><p class="para" id="N65541">Summertime temperatures at the surfaces of barren maritime Antarctic soils can approach or exceed 20°C under cloudless skies around solar noon. Here we show that the metabolism of the cold‐adapted and widespread Antarctic soil fungus <i>Pseudogymnoascus roseus</i> is inhibited when it is exposed to temperatures cycling daily to more than 20°C, both in the natural environment and the laboratory, with substantial reductions in the in vitro growth rates of colonies and activities of extracellular enzymes. We propose that surface warming in cold regions has the potential to inhibit the growth of other cold‐adapted microbes, with negative effects on soils as the Earth's climate continues to warm.<div class="section"><div class="box" id="N65546"><div class="imageVideo"><img src="/dataresources/secured/content-1765944227358-894beeff-cdd4-45e9-b375-5b4025cd8466/assets/GCB-27-1111-g007.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-12-18T00:00]]></pubDate>
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            <title><![CDATA[Nitrogen cycling microbiomes are structured by plant mycorrhizal associations with consequences for nitrogen oxide fluxes in forests]]></title>
            <media:thumbnail url="https://storage.googleapis.com/nova-demo-unsecured-files/unsecured/content-1765942228990-167e992f-c099-4d93-9587-5f9654f42903/cover.png"></media:thumbnail>
            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15439</link>
            <description><![CDATA[<p class="para" id="N65542">Volatile nitrogen oxides (N<sub>2</sub>O, NO, NO<sub>2</sub>, HONO, …) can negatively impact climate, air quality, and human health. Using soils collected from temperate forests across the eastern United States, we show microbial communities involved in nitrogen (N) cycling are structured, in large part, by the composition of overstory trees, leading to predictable N‐cycling syndromes, with consequences for emissions of volatile nitrogen oxides to air. Trees associating with arbuscular mycorrhizal (AM) fungi promote soil microbial communities with higher N‐cycle potential and activity, relative to microbial communities in soils dominated by trees associating with ectomycorrhizal (ECM) fungi. Metagenomic analysis and gene expression studies reveal a 5 and 3.5 times greater estimated N‐cycle gene and transcript copy numbers, respectively, in AM relative to ECM soil. Furthermore, we observe a 60% linear decrease in volatile reactive nitrogen gas flux (NO<i><sub>y</sub></i> ≡ NO, NO<sub>2</sub>, HONO) as ECM tree abundance increases. Compared to oxic conditions, gas flux potential of N<sub>2</sub>O and NO increase significantly under anoxic conditions for AM soil (30‐ and 120‐fold increase), but not ECM soil—likely owing to small concentrations of available substrate (NO3‐) in ECM soil. Linear mixed effects modeling shows that ECM tree abundance, microbial process rates, and geographic location are primarily responsible for variation in peak potential NO<sub>y</sub> flux. Given that nearly all tree species associate with either AM or ECM fungi, our results indicate that the consequences of tree species shifts associated with global change may have predictable consequences for soil N cycling.</p><p class="para" id="N65541">Volatile nitrogen oxides can negatively impact climate, air quality, and human health. Using soils collected from temperate forests across the eastern United States, we show microbial communities involved in nitrogen (N) cycling are structured, in large part, by the composition of overstory trees, leading to predictable N cycling syndromes, with consequences for emissions of volatile nitrogen oxides to air. Trees associating with arbuscular mycorrhizal (AM) fungi promote soil microbial communities with higher N‐cycle potential and activity, relative to microbial communities in soils dominated by trees associating with ectomycorrhizal (ECM) fungi. Given that nearly all tree species associate with either AM or ECM fungi, our results indicate that the consequences of tree species shifts associated with global change may have predictable consequences for soil N cycling.<div class="section"><div class="box" id="N65543"><div class="imageVideo"><img src="/dataresources/secured/content-1765942228990-167e992f-c099-4d93-9587-5f9654f42903/assets/GCB-27-1068-g010.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-12-15T00:00]]></pubDate>
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            <title><![CDATA[A physiology‐based Earth observation model indicates stagnation in the global gross primary production during recent decades]]></title>
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            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15424</link>
            <description><![CDATA[<p class="para" id="N65542">Earth observation‐based estimates of global gross primary production (GPP) are essential for understanding the response of the terrestrial biosphere to climatic change and other anthropogenic forcing. In this study, we attempt an ecosystem‐level physiological approach of estimating GPP using an asymptotic light response function (LRF) between GPP and incoming photosynthetically active radiation (PAR) that better represents the response observed at high spatiotemporal resolutions than the conventional light use efficiency approach. Modelled GPP is thereafter constrained with meteorological and hydrological variables. The variability in field‐observed GPP, net primary productivity and solar‐induced fluorescence was better or equally well captured by our LRF‐based GPP when compared with six state‐of‐the‐art Earth observation‐based GPP products. Over the period 1982–2015, the LRF‐based average annual global terrestrial GPP budget was 121.8 ± 3.5 Pg C, with a detrended inter‐annual variability of 0.74 ± 0.13 Pg C. The strongest inter‐annual variability was observed in semi‐arid regions, but croplands in China and India also showed strong inter‐annual variations. The trend in global terrestrial GPP during 1982–2015 was 0.27 ± 0.02 Pg C year<sup>−1</sup>, and was generally larger in the northern than the southern hemisphere. Most positive GPP trends were seen in areas with croplands whereas negative trends were observed for large non‐cropped parts of the tropics. Trends were strong during the eighties and nineties but levelled off around year 2000. Other GPP products either showed no trends or continuous increase throughout the study period. This study benchmarks a first global Earth observation‐based model using an asymptotic light response function, improving simulations of GPP, and reveals a stagnation in the global GPP after the year 2000.</p><p class="para" id="N65541">A novel modelling approach for Earth observation of global gross primary production (GPP) of vegetation was introduced. The model improved simulations of GPP, and revealed a stagnation in the global GPP after the year 2000.<div class="section"><div class="box" id="N65543"><div class="imageVideo"><img src="/dataresources/secured/content-1765939397552-57dcb881-207d-4321-aa44-397874fcca01/assets/GCB-27-836-g008.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-12-06T00:00]]></pubDate>
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            <title><![CDATA[Multi‐hypothesis comparison of Farquhar and Collatz photosynthesis models reveals the unexpected influence of empirical assumptions at leaf and global scales]]></title>
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            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15366</link>
            <description><![CDATA[<p class="para" id="N65542">Mechanistic photosynthesis models are at the heart of terrestrial biosphere models (TBMs) simulating the daily, monthly, annual and decadal rhythms of carbon assimilation (<i>A</i>). These models are founded on robust mathematical hypotheses that describe how <i>A</i> responds to changes in light and atmospheric CO<sub>2</sub> concentration. Two predominant photosynthesis models are in common usage: Farquhar (FvCB) and Collatz (CBGB). However, a detailed quantitative comparison of these two models has never been undertaken. In this study, we unify the FvCB and CBGB models to a common parameter set and use novel multi‐hypothesis methods (that account for both hypothesis and parameter variability) for process‐level sensitivity analysis. These models represent three key biological processes: carboxylation, electron transport, triose phosphate use (TPU) and an additional model process: limiting‐rate selection. Each of the four processes comprises 1–3 alternative hypotheses giving 12 possible individual models with a total of 14 parameters. To broaden inference, TBM simulations were run and novel, high‐resolution photosynthesis measurements were made. We show that parameters associated with carboxylation are the most influential <i>parameters</i> but also reveal the surprising and marked dominance of the limiting‐rate selection <i>process</i> (accounting for 57% of the variation in <i>A</i> vs. 22% for carboxylation). The limiting‐rate selection assumption proposed by CBGB smooths the transition between limiting rates and always reduces <i>A</i> below the minimum of all potentially limiting rates, by up to 25%, effectively imposing a fourth limitation on <i>A</i>. Evaluation of the CBGB smoothing function in three TBMs demonstrated a reduction in global <i>A</i> by 4%–10%, equivalent to 50%–160% of current annual fossil fuel emissions. This analysis reveals a surprising and previously unquantified influence of a process that has been integral to many TBMs for decades, highlighting the value of multi‐hypothesis methods.</p><p class="para" id="N65541">Leaf photosynthesis models are the beating heart of global carbon cycle models, simulating the rhythms of CO<sub>2</sub> transfer from the atmosphere to plants. Two key photosynthesis model variants are commonly used: the Farquhar and Collatz models, which vary in the way that some subprocesses are represented. Despite their almost ubiquitous use, the consequences of these alternative choices has never been formally investigated. Here we apply novel multi‐hypothesis modelling methods to investigate the influence of 14 parameters and four processes with alternative representations in photosynthesis models, finding the surprising dominance of a process that has not been extensively evaluated with data.<div class="section"><div class="box" id="N65546"><div class="imageVideo"><img src="/dataresources/secured/content-1765933705292-7492027a-806f-4e4e-9902-1c50526877ec/assets/GCB-27-804-g006.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-10-31T00:00]]></pubDate>
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            <title><![CDATA[Species sensitivities to a global pollutant: A meta‐analysis on acoustic signals in response to anthropogenic noise]]></title>
            <media:thumbnail url="https://storage.googleapis.com/nova-demo-unsecured-files/unsecured/content-1765839261543-f3adc171-67f2-42cc-b886-fd7fc931a479/cover.png"></media:thumbnail>
            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15428</link>
            <description><![CDATA[<p class="para" id="N65542">Anthropogenically driven environmental changes affect our planet at an unprecedented rate. Among these changes are those in the acoustic environment caused by anthropogenic noise, which can affect both animals and humans. In many species, acoustic communication plays a crucial role to maintain social relationships by exchanging information via acoustic signals. However, how species relying on acoustic communication differ in their adjustments to anthropogenic noise is little understood. Yet, this is crucial because protecting species effectively depends on our capability to predict how species differ in their response to human‐induced environmental changes. Using a phylogenetically controlled meta‐analysis, we quantified differences in adjustments of acoustic signals to anthropogenic noise among species. The effect sizes included in the analysis were obtained from noise exposure experiments, as only carefully controlled experiments allow to establish cause‐and‐effect relationships. We found that animals changed acoustic signals when exposed to noise, but the magnitude and the direction of adjustments differed among species. Given the importance of communication in the animal kingdom, these adjustments can affect social relationships in many species. The diversity of responses among species highlights the necessity to assess the effect of environmental stressors not only for a few species, because an effect may be positive in one species but negative in another depending on the species’ biology. Thus, an effective conservation approach to protect different species is to preserve natural soundscapes of ecosystems to which species have adapted to by reducing or mitigating the emission of anthropogenic noise into the environment.</p><p class="para" id="N65541">Using a phylogenetically controlled meta‐analysis, we quantified differences in adjustments of acoustic signals to anthropogenic noise. We found that animals changed acoustic signals when experimentally exposed to noise, but the magnitude and the direction of adjustments differed among species. Thus, an effective conservation approach to protect different species is to preserve natural soundscapes of ecosystems to which species have adapted to by reducing or mitigating the emission of anthropogenic noise into the environment.<div class="section"><div class="box" id="N65543"><div class="imageVideo"><img src="/dataresources/secured/content-1765839261543-f3adc171-67f2-42cc-b886-fd7fc931a479/assets/GCB-27-675-g008.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-12-01T00:00]]></pubDate>
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            <title><![CDATA[A century of coping with environmental and ecological changes via compensatory biomineralization in mussels]]></title>
            <media:thumbnail url="https://storage.googleapis.com/nova-demo-unsecured-files/unsecured/content-1765833939062-4e622d4c-3cbc-42aa-9648-a8fd3291ed8a/cover.png"></media:thumbnail>
            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15417</link>
            <description><![CDATA[<p class="para" id="N65542">Accurate biological models are critical to predict biotic responses to climate change and human‐caused disturbances. Current understanding of organismal responses to change stems from studies over relatively short timescales. However, most projections lack long‐term observations incorporating the potential for transgenerational phenotypic plasticity and genetic adaption, the keys to resistance. Here, we describe unexpected temporal compensatory responses in biomineralization as a mechanism for resistance to altered environmental conditions and predation impacts in a calcifying foundation species. We evaluated exceptional archival specimens of the blue mussel <i>Mytilus edulis</i> collected regularly between 1904 and 2016 along 15 km of Belgian coastline, along with records of key environmental descriptors and predators. Contrary to global‐scale predictions, shell production increased over the last century, highlighting a protective capacity of mussels for qualitative and quantitative trade‐offs in biomineralization as compensatory responses to altered environments. We also demonstrated the role of changes in predator communities in stimulating unanticipated biological trends that run contrary to experimental predictive models under future climate scenarios. Analysis of archival records has a key role for anticipating emergent impacts of climate change.</p><p class="para" id="N65541">Current understanding of organismal responses to change stems from relatively short‐term studies. Most projections lack long‐term observations incorporating the potential for transgenerational phenotypic plasticity and genetic adaption. We describe unexpected temporal responses in biomineralization as a mechanism for resistance to altered environments in the blue mussel <i>Mytilus edulis</i>. We evaluated archival mussel specimens collected regularly between 1904 and 2016, along with records of environmental descriptors and predators. Contrary to global‐scale predictions, shell production increased over the last century, highlighting a protective capacity of mussels for qualitative and quantitative trade‐offs in biomineralization as compensatory responses to altered environments and predator communities.<div class="section"><div class="box" id="N65546"><div class="imageVideo"><img src="/dataresources/secured/content-1765833939062-4e622d4c-3cbc-42aa-9648-a8fd3291ed8a/assets/GCB-27-624-g007.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-11-21T00:00]]></pubDate>
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            <title><![CDATA[What’s hot and what’s not: Making sense of biodiversity ‘hotspots’]]></title>
            <media:thumbnail url="https://storage.googleapis.com/nova-demo-unsecured-files/unsecured/content-1765821010555-309e9d45-77e2-44d1-8872-465c2cfeb645/cover.png"></media:thumbnail>
            <link>https://www.novareader.co/book/isbn/10.1111/gcb.15443</link>
            <description><![CDATA[<p class="para" id="N65542">Conserving biogeographic regions with especially high biodiversity, known as biodiversity ‘hotspots’, is intuitive because finite resources can be focussed towards manageable units. Yet, biodiversity, environmental conditions and their relationship are more complex with multidimensional properties. Assessments which ignore this risk failing to detect change, identify its direction or gauge the scale of appropriate intervention. Conflicting concepts which assume assemblages as either sharply delineated communities or loosely collected species have also hampered progress in the way we assess and conserve biodiversity. We focus on the marine benthos where delineating manageable areas for conservation is an attractive prospect because it holds most marine species and constitutes the largest single ecosystem on earth by area. Using two large UK marine benthic faunal datasets, we present a spatially gridded data sampling design to account for survey effects which would otherwise be the principal drivers of diversity estimates. We then assess γ‐diversity (regional richness) with diversity partitioned between α (local richness) and β (dissimilarity), and their change in relation to covariates to test whether defining and conserving biodiversity hotspots is an effective conservation strategy in light of the prevailing forces structuring those assemblages. α‐, β‐ and γ‐diversity hotspots were largely inconsistent with each metric relating uniquely to the covariates, and loosely collected species generally prevailed with relatively few distinct assemblages. Hotspots could therefore be an unreliable means to direct conservation efforts if based on only a component part of diversity. When assessed alongside environmental gradients, α‐, β‐ and γ‐diversity provide a multidimensional but still intuitive perspective of biodiversity change that can direct conservation towards key drivers and the appropriate scale for intervention. Our study also highlights possible temporal declines in species richness over 30 years and thus the need for future integrated monitoring to reveal the causal drivers of biodiversity change.</p><p class="para" id="N65541">Conserving biodiversity ‘hotspots’ is intuitive because finite resources can be focussed towards manageable units. Yet, biodiversity, environmental conditions and their relationship are more complex with multidimensional properties. Assessments which ignore this risk failing to detect change, identify its direction, or gauge the scale of appropriate intervention. We focus on the marine benthos which holds most marine species and constitutes the largest single ecosystem on earth by area. When assessed alongside environmental gradients, α‐, β‐ and γ‐diversity provide a multidimensional but still intuitive perspective of biodiversity change that can direct conservation towards key drivers and the appropriate scale for intervention. Photographs used are a combination of © Elena Couce and © Crown Copyright, the latter collected by Cefas, Cornwall IFCA and Environment Agency whilst undertaking survey work in partnerships with the JNCC and Natural England.<div class="section"><div class="box" id="N65543"><div class="imageVideo"><img src="/dataresources/secured/content-1765821010555-309e9d45-77e2-44d1-8872-465c2cfeb645/assets/GCB-27-521-g007.jpg" alt=""/></div></div></div>
</p>]]></description>
            <pubDate><![CDATA[2020-11-26T00:00]]></pubDate>
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