.Modern dendroecological studies integrate aspects of
historical climatology, ecosystem productivity, plant physi-
ology, and wood anatomy. Mounting evidence, for instance,
compels local- to large-scale approaches, biometric and
eddy-covariance calculations, high-resolution dendrometer
measurements, as well as quantitative wood anatomical
parameters, with the latter providing detailed insight on
the intra-annual course of cell formation. Meanwhile,
advancements in mycological research that focus on long-
term monitoring settings and data mining initiatives, en-
able – at least to a certain degree – changes in fungal
phenology and productivity to be linked with local- to syn-
optic-scale temperature and/or hydroclimatic variability [5–
11]. Meteorological influences, however, may only explain some of the observed variation in fungal phenology and
productivity, implying other factors to be considered. Host
plants are crucial for carbon partitioning mechanisms, be-
cause large fractions of the photosynthetically fixed carbon
are directed below ground to the associated mycorrhizal
fungi [12]. Tree growth is thus key in governing mycorrhizal
mushrooms. In this regard, new genome analyses and tran-
scriptomics appear promising to provide further insight on a
wide range of functional aspects related to the fungus–host
symbiosis [13]. Moreover, next-generation sequencing tech-
niques illuminate the below-ground structure and richness
of fungal communities [14], and emphasize the ecological
importance of common mycelial networks, as well as the
relative role mycorrhizal fungi and their perennial partners
play in carbon metabolizing [15,16]. Although the yet-sepa-
rated disciplines of dendroecology, wood anatomy, and my-
cology generally operate on different timescales, recent
endeavors in all of these fields suggest unexpected synergies
to arise when combining them. Latest advancement in the
precision and interpretation of tree-ring chronologies, to-
gether with the performance of quantitative wood anatomy
that has been consequently supplemented by intra-annual
dendrometer measurements, as well as the new awareness
from long-term observational networks of mushroom and
mycelial formation, are all indicative of a wide range of
methodological and scientific overlap.
.Modern dendroecological studies integrate aspects ofhistorical climatology, ecosystem productivity, plant physi-ology, and wood anatomy. Mounting evidence, for instance,compels local- to large-scale approaches, biometric andeddy-covariance calculations, high-resolution dendrometermeasurements, as well as quantitative wood anatomicalparameters, with the latter providing detailed insight onthe intra-annual course of cell formation. Meanwhile,advancements in mycological research that focus on long-term monitoring settings and data mining initiatives, en-able – at least to a certain degree – changes in fungalphenology and productivity to be linked with local- to syn-optic-scale temperature and/or hydroclimatic variability [5–11]. Meteorological influences, however, may only explain some of the observed variation in fungal phenology andproductivity, implying other factors to be considered. Hostplants are crucial for carbon partitioning mechanisms, be-cause large fractions of the photosynthetically fixed carbonare directed below ground to the associated mycorrhizalfungi [12]. Tree growth is thus key in governing mycorrhizalmushrooms. In this regard, new genome analyses and tran-scriptomics appear promising to provide further insight on awide range of functional aspects related to the fungus–hostsymbiosis [13]. Moreover, next-generation sequencing tech-niques illuminate the below-ground structure and richnessof fungal communities [14], and emphasize the ecologicalimportance of common mycelial networks, as well as therelative role mycorrhizal fungi and their perennial partnersplay in carbon metabolizing [15,16]. Although the yet-sepa-rated disciplines of dendroecology, wood anatomy, and my-cology generally operate on different timescales, recentendeavors in all of these fields suggest unexpected synergiesto arise when combining them. Latest advancement in theprecision and interpretation of tree-ring chronologies, to-gether with the performance of quantitative wood anatomythat has been consequently supplemented by intra-annualdendrometer measurements, as well as the new awarenessfrom long-term observational networks of mushroom andmycelial formation, are all indicative of a wide range ofmethodological and scientific overlap.
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