580 Pflanzen (Botanik)
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Forests influence the climate of our Earth and provide habitat and food for many species and resources for human use. These valuable ecosystems are threatened by fast environmental changes caused by human-induced climte change. Negative growth responses and higher tree mortality rates were associated with increasing physiological stress induced by global warming. Especially boreal forests at high latitudes in the arctic region are threatened, a region predicted to undergo the highest increase in temperature during the next decades. Therefore, it is important to assess the adaptation potential in trees. For this purpose, I studied natural populations of white spruce (Picea glauca (Moench) Voss) in Alaska. In this thesis, I present three scientific papers in which my co-authors and I studied the phenotypic plasticity and genetic basis of tree growth, wood anatomy and drought tolerance as well as the genetic structure of white spruce populations in contrasting environments. We established three sites representing two cold-limited treelines and one drought-limited treeline with a paired plot design including one plot located at the treeline and one plot located in a closed-canopy forest, respectively. Additionally, the study design included one forest plot as reference. Within the entire project, in total 3,000 trees were measured, genotyped and dendrochronological data was obtained. I used several approaches to estimate the neutral and adaptive genetic diversity and phenotypic plasticity of white spruce as a model organism to explore the adaptation potential of trees to climate change.
In the first chapter, I combined neutral genetic markers with dendrochronological and climatic data to investigate population structure and individual growth of white spruce. Several individual-based dendrochronological approaches were applied to test the influence of genetic similarity and microenvironment on growth performance. The white spruce populations of the different sites showed high gene flow and high genetic diversity within and low genetic differentiation among populations, rather explained by geographic distance. The individual growth performances showed a high plasticity rather influenced by microenvironment than genetic similarity.
In the second chapter, I investigated the populations of the drought and cold-limited treeline sites to decipher the underlying genetic structure of drought tolerance using different genotype-phenotype association analyses. Based on tree-ring series and climatic data, growth declines caused by drought stress were identified and the individual reaction to the drought stress event was determined. A subset of 458 trees was genotyped, using SNPs in candidate genes and associated with the individual drought response. Most of the associations were revealed by an approach which took into account small-effect size SNPs and their interactions. Populations of the contrasting treelines responded differently to drought stress events. Populations further showed divergent genetic structures associated with drought responsive traits, most of them in the drought-limited site, indicating divergent selection pressure.
In the third chapter, my co-authors and I studied xylem anatomical traits at one of the cold-limited treeline sites to investigate whether genetic or spatial grouping affected the anatomy and growth of white spruce. Annual growth and xylem anatomy were compared between spatial groups and between genetic groups and individuals. Overall, wood traits were rather influenced by spatial than genetic grouping. Genetic effects were only found in earlywood hydraulic diameter and latewood density. Environmental conditions indirectly influenced traits related to water transport.
In conclusion, white spruce showed a high genetic diversity within and a low genetic differentiation among populations influenced by high gene flow rates. Genetic differences among populations are rather caused by geographical distance and therefore genetic drift. Differing selection pressure at the treeline ecotones presumably lead to divergent genetic structures underlying drought-tolerant phenotypes among the populations. Thus, adaptation to drought most likely acts on a local scale and involves small frequency shifts in several interacting genes. The identified genes with adaptive growth traits can be used to further exlore local adaptation in white spruce. Tree growth and wood anatomical traits are rather influenced by the environment than genetics and showed a high phentoypic plasticity. The high genetic diverstiy and phenotypic plasticity of white spruce may help the species to cope with rapid environmental changes. Still, additional work is needed to further explore adaptation processes to estimate how tree species reacted to rapid climate change. The presented thesis shed some light on the adaptation potential of trees by the example of white spruce using several approaches.
Myxomycetes or Myxogastria (supergroup Amoebozoa) are one of several Protistean groups dispersing via airborne spores. The model organism for the group, so far exclusively studied in a laboratory environment, is Physarum polycephalum. Here, molecular evolution, distribution and the ecology of spores dispersal was investigated for the non-model species Physarum albescens. This nivicolous myxomycete fruits with snow melt in most mountain ranges of the northern hemisphere and disperses via spherical, dark-colored and melanin-rich spores. Fruit body development and subsequent spore dispersal occurs within a short time window of a few days. At this time, the fruiting plasmodium is fully exposed to the harsh environment if the protecting snow melts away. The spores, with a diameter of 10–13 µm of the typical size for myxomycetes, can potentially reach all suitable habitats worldwide, which led to the assumption that not only Ph. albescens but most myxomycete species should be ubiquitously distributed over the world.
In the first part of this study (article 1), the question was, if spore dispersal can realize a gene flow sufficient to meet the above-mentioned assumption. A total of 324 accessions of Ph. albescens, collected all over the northern hemisphere, was sequenced for 1-3 genetic markers (SSU, EF1A, COI), and 98 specimens were further analyzed using the genotyping by sequencing technique. As a result, at least 18 reproductively isolated units, which can be seen as cryptic biological species, emerged as phylogroups in a three-gene phylogeny, but as well in a SNP-based phylogeny and were confirmed by a recombination analysis between the three markers. However, this evolutive radiation is not simply caused by geographic fragmentation due to low dispersal capability: within a certain region, multiple phylogroups coexisted next to each other, although some appeared to be regional endemics. Most likely, mutations in mating-type genes, as shown to exist for the cultivable Ph. polycephalum, are the main drivers of speciation. This challenges the hypothesis of ubiquitous distribution of Ph. albescens and corroborates the results of the few available studies for other myxomycete species. In addition, groups of clonal specimens, mostly but not always restricted to a certain slope or valley indicated that sexual and asexual reproduction coexists in the natural populations of Ph. albescens.
In the second part (articles 2), the fundamental niche for Ph. albescens was described using all available records for the species. The resulting set of 537 unique occurrence points was subjected to a correlative spatial approach using the software MaxEnt. In dependence on the predictor variables three species distribution models emerged which differed only in details. The first consisted of only 19 bioclimatic variables and an elevation map from the WorldClim dataset. The second was corrected for pseudo-absences resulting from missing survey activities, and the third was expanded with an additional categorical environment variable on snow cover. High mean AUC (area under the curve) values above 0.97 could be reached with all three models. Variables for snow cover, precipitation of the coldest quarter (of the year), and elevation correlated highly to predict the distribution of Ph. albescens. Only in mid-northern latitudes, elevation alone was a good predictor, but it would cause false-positive predictions in arid mountain ranges and failed to explain occurrence in lowland sites at higher latitudes. Mountains in humid climates showed the highest incidences, confirming recent studies that long-lasting snow covers combined with mild summers are crucial for the ecological guild of nivicolous myxomycetes, with Ph. albescens as a typical species.
Spore size is crucial for dispersal ability and should thus be a character under strong selection. In addition, spores carrying two nuclei with opposite mating types should have a colonization advantage. This was the hypothesis for the last part of this study (articles 3 and 4), which investigated this trait in a quantitative manner. This required a method to analyze thousands of spores automatically (article 3) and with high precision for size and the number of nuclei enclosed. Human errors should be excluded, to reveal even subtle differences in the resulting spore size distributions. Two challenges had to be met for this approach. First, a preparation technique was developed to reduce false segmentations due to overlaying spores by aligning spores on one common plane with a high-frequency vibration device. Second, the segmentation process was automated to allow separating spores that are densely packed in the respective images. A machine learning algorithm was set up and trained to reliable identify and measure dark-colored spores. The technique produced consistent results with high accuracy, and the large number of spores allowed to compile spore size distributions, to check for the constancy of this character, which is impossible with manual measurements limited to low numbers.
The resulting spore size distributions, obtained from over 80 specimens (article 4), were mostly narrow, which is in accordance with our hypothesis. Spore size was as well fairly constant within fructifications from one colony. However, mean spore size within different accessions of Ph. albescens showed large variation (ca. 10%, a range often indicated to key out different morphospecies of myxomycetes), and this was explained only by a minor part with differences between biospecies. Not much smaller (8%) was the variation within a group of clonal specimens collected within 25 m distance. This points to a strong influence of environmental factors even at a micro spatial scale, perhaps caused by microclimatic differences and high phenotypic plasticity for spore size. The influence of large-scale covariates like altitude or latitude was negligible. However, spore size correlated with the variance in this trait, indicating that oversized spores may be caused by detrimental environmental conditions. Two aberrations in spore development were found: First, a few specimens showed a multimodal distribution for spore size with two or even three discernible spore populations. The estimated volumes of those populations correspond to a multiple of the first and most abundant conspicuous spore size population. Second, not all spores were uninucleate as to be expected for meiotic products. This was revealed by fluorescence signals from staining the same spores with DAPI, with a second machine learning algorithm trained to identify the nuclei in a spore. A few specimens showed a significant proportion of binucleated spores in the size range of normal-sized ones, and these specimens were not the ones with multimodal spore size distributions. This indicates that the negative impacts (inbreeding) of multinucleate spores should outweigh a possible colonization advantage and is in accordance with the high genetic diversity found in the worldwide population of Ph. albescens, indicating predominantly sexual reproduction in wild populations of myxomycetes.
Forests are ecologically important ecosystems, for example, they absorb CO2 from the
atmosphere, mitigate climate change, and constitute habitats for the majority of terrestrial
flora and fauna. Currently, due to increasing human pressure, forest ecosystems are
increasingly subjected to changing environmental conditions, which may alter forest growth
to varying degrees. However, how exactly different tree species will respond to climate
change remains uncertain and requires further comprehensive studies performed at different
spatial scales and using various tree-ring parameters.
This dissertation aims to advance the knowledge about tree-ring densitometry and
tree responses to climate variability and extremes at different spatial scales, using various
tree species. More specifically, the following aims are pursued: (i) to obtain and compare
wood density data using different techniques, and to assess variability among laboratories
(Chapter I). (ii) To investigate microsite effects on local and regional Scots pine (Pinus
sylvestris L.) responses to climate variability (Chapter II) and extremes (Chapter III),
using ring width (RW) and latewood blue intensity (LBI) parameters. (iii) To give a general
site- and regional-scales overview of Scots pine, pedunculate oak (Quercus robur L.), and
European beach (Fagus sylvatica L.) RW responses to climate variability (Chapter IV). (iv)
To discuss the challenges which may result from compiling tree ring records from different
(micro)sites into large-scale networks. The study area comprises nine coastal dune sites, each
represented by two contrasting microsites: dune ridge and bottom (Chapters II and III), and
310 different sites within the south Baltic Sea lowlands (Chapter IV).
The dissertation confirms that sample processing and wood density measuring are
very important steps, which, if not performed carefully, may result in biases in growth trends,
climate-growth responses, and climate reconstructions. The performed experiment proved
that the mean levels of different wood density-related parameters are never comparable due
to different measurement resolutions between various techniques and laboratories. Further,
the study revealed substantial biases using data measured from rings of varying width due
to resolution issues, where resolution itself and wood density are lowered for narrow rings
compared to wide rings (Chapter I).
The (micro)site-specific investigation showed that, depending on the species,
different climate variables (temperature, precipitation, or drought) constitute important
factors driving tree growth across investigated locations (Chapters II and IV). However,
there is evidence that the strength and/or direction of climate-growth responses differ(s)
between microsite types (Chapter II) and across sites (Chapter IV). Moreover, climategrowth
responses are non-stationary over time regardless of the tree species and tree-ring
parameter used in the analysis (Chapters II and IV). There are also differences in RW and
LBI responses to extreme events at dune ridge and bottom microsites (Chapter III).
The regional-scale investigations revealed that climate-growth responses (strength
and non-stationarity) are quite similar to those observed at the local scale. However,
compiling RW or LBI measurements into regional networks to study tree responses to
extreme events led to weakened signals (Chapter III).
The findings presented in Chapters II and IV suggest that the strength, direction,
and non-stationary responses are very likely caused by several climatic and non-climatic
factors. The mild climate in the south Baltic Sea region presumably does not constitute a
leading limiting growth factor, especially for Scots pine, whose distribution extends from
southern to northern Europe. Thus, the observed climate-growth responses are usually of
weak to moderate strength. In contrast, for other species reaching their distribution limit at
the Baltic coast, the climatic signal can be very strong. However, the observed findings also
result from the effects of microsite conditions, and potentially other factors (e.g.,
management, stand dynamic), which all together alter the physiological response of the tree
at a local scale. Although climate at the south Baltic Sea coast is mild, extreme climate events
may occur and affect tree growth. As demonstrated (Chapter III), extreme climate events
affected tree growth across dune sites, however, to varying degrees. The prominent
differences in tree responses to extreme climate events were significant at the local scale but
averaged out at the regional scale. This is very likely associated with observed microsite
differences, where each microsite experiences different drivers and dynamics of extreme
growth reductions.
This dissertation helped to demonstrate that integrating local tree-ring records into
regional networks involves a series of challenges, which arise at different stages of research.
In fact, not all possible challenges have been discussed in this dissertation. However, it can
be summarized that several steps performed first at the local scale are very important for the
quality and certainty of climate-growth responses, tracking tree recovery after extreme
events, and potential climate reconstructions at the larger scale. Among them, identification
of microsite conditions, sample preparation, and measurement, examination of growth
patterns and trends, and identification of a common limiting growth factor are very
important. Otherwise, the compilation of various tree-ring data into a single dataset could
lead to over- or underestimation of the results and biased interpretations.
In the search for alternative treatment options for infections with multi-resistant germs,
traditionally used medicinal plants are currently being examined more intensively. In this study,
the antimicrobial and anti-biofilm activities of 14 herbal drugs were investigated. Nine of the tested
drugs were traditionally used in Europe for treatment of local infections. For comparison, another
five drugs monographed in the European Pharmacopoeia were used. Additionally, the total tannin
and flavonoid contents of all tested drugs were analyzed. HPLC fingerprints were recorded to ob-
tain further insights into the components of the extracts. The aim of the study was to identify herbal
drugs that might be useable for treatment of infectious diseases, even with multidrug resistant E.
coli, and to correlate the antimicrobial activity with the total content of tannins and flavonoids. The
agar diffusion test and anti-biofilm assay were used to evaluate the antimicrobial potential of dif-
ferent extracts from the plants. Colorimetric methods (from European Pharmacopeia) were used for
determination of total tannins and flavonoids. The direct antimicrobial activity of most of the tested
extracts was low to moderate. The anti-biofilm activity was found to be down to 10 µg mL −1 for
some extracts. Tannin contents between 2.2% and 10.4% of dry weight and total flavonoid contents
between 0.1% and 1.6% were found. Correlation analysis indicates that the antimicrobial and the
anti-biofilm activity is significantly (p < 0.05) dependent on tannin content, but not on flavonoid
content. The data analysis revealed that tannin-rich herbal drugs inhibit pathogens in different
ways. Thus, some of the tested herbal drugs might be useable for local infections with multi-re-
sistant biofilm-forming pathogens. For some of the tested drugs, this is the first report about anti-
biofilm activity, as well as total tannin and flavonoid content.
Forest ecosystems around the world and especially boreal forests, are facing
drastically changing climatic conditions. It is known that these changes could
challenge their functionality and vitality. Still, the exact impact is not fully
understood, as tree growth is a complex process and depends on countless
environmental and genetic factors. To estimate the effects of climate change
on tree growth and forest development precisely, we must learn more about
tree growth itself. A comprehensive approach is needed where trees and
forests are investigated on different scales and levels of detail, ranging from
global studies to studies on single individuals.
In this dissertation, I follow such a comprehensive approach, using the
North American conifer white spruce as an example. I present three papers
in the form of three chapters in which my co-authors and I studied the
growth and anatomy of white spruce (Picea glauca [Moench] Voss) and how
it is influenced by environmental, climatic, and genetic factors.
We used diverse approaches and methods on different spatial scales, ranging from
investigations on the landscape to the local scale. We established three paired
plots with forest and treeline sites (two cold-limited and one drought-limited).
as well as one additional forest site. In the first chapter, we concentrated
on the genetic diversity of white spruce within and between populations at
all study sites throughout Alaska. The genetic investigations were combined
with analyses on the individual growth response of trees to climatic conditions
to find whether genetic similarities or spatial proximity caused similarities
in growth and climatic sensitivity. In the second chapter, we studied the
direct and indirect effects of environmental conditions on the xylem tissue
of white spruce. We analyzed the impact of precipitation, temperature, and
tree height on four xylem anatomical traits in trees growing at the three
treelines. The investigated traits represented the main functions of xylem
tissue (i.e., water transport and structural support). In the third chapter,
we investigated similar xylem anatomical traits at one cold-limited treeline.
We compared xylem anatomy and annual increment between genetic groups
and individuals and between spatial groups to investigate whether spatial or
genetic grouping influenced the anatomy and growth of white spruce.
We found an overall high gene flow and high genetic diversity in white
spruce. However, the sensitivity of the growth and anatomical traits of white
spruce was driven mainly by spatial rather than genetic effects and differed
between study sites. Trees from the drought-limited site were more sensitive
towards precipitation and a moisture index, while trees from the cold-limited
sites were more sensitive towards temperature. A strong direct effect of tem-
perature was primarily found in latewood traits related to the structural sup-
port of the tree. Earlywood traits related to water transport, however, were
influenced mainly by tree height. Tree height itself was potentially affected
by diverse abiotic and biotic factors (e.g., (micro)climate, soil conditions,
and competition). Thus, traits related to water transport were indirectly
influenced by environmental conditions. Genetic effects in xylem anatomical
traits were found in the earlywood hydraulic diameter and latewood den-
sity, whereas in general, primarily spatial rather than genetic grouping was
influencing the anatomy of white spruce.
Overall, white spruce showed to be a genetically diverse species with a
high gene flow. The effects of spatial proximity and spatial grouping on the
sensitivity and anatomy of white spruce indicate high phenotypic plastic-
ity. This high phenotypic plasticity combined with the vast genetic diversity
translates into an immense potential for the species to adjust (phenotypically)
and possibly adapt (genetically) to changing conditions. Thus, in terms of
climate change, white spruce may be a rather persistent species that manages
to cope with the drastic changes. Though additional work might be needed to
draw a more solid conclusion, the presented work shows how a comprehensive
study approach can help to interpret and understand the growth and ecology
of a tree species. It may be an inspiration for future studies to broaden their
approaches and to use comprehensive methods on different levels of detail to
not only observe trees but to explore and understand them.
In Mitteleuropa kommen innerhalb der Gattung Diphasiastrum neben drei Ausgangsarten (D. alpinum, D. complanatum, D. tristachyum) drei Taxa hybridogenen Ursprungs vor (D. x issleri = D. alpinum x D. complanatum; D. x oellgaardii = D. alpinum x D. tristachyum; D. x zeilleri = D. complanatum x D. tristachyum). Alle sechs Taxa sind diploid. Die homoploiden Hybriden unterscheiden sich sowohl morphologisch als auch hinsichtlich ihres Kern-DNA-Gehaltes deutlich voneinander und nehmen eine intermediäre Stellung zwischen ihren Elternarten ein. Daher ist zu vermuten, dass es genetische Schranken für Rückkreuzungen gibt. Außer den regelmäßig auftretenden diploiden Hybriden konnten drei sehr seltene triploide Diphasiastrum-Hybriden nachgewiesen werden. Auf Grund ihres Kern-DNA-Gehaltes und der Morphologie kann auf folgende Kombinationen geschlossen werden:
Diphasiastrum alpinum x D. x issleri (Genomformel AAC),
Diphasiastrum alpinum x D. x oellgaardii (Genomformel AAT),
Diphasiastrum complanatum ssp. complanatum x D. x issleri (Genomformel ACC).
Es kann vermutet werden, dass diese triploiden Hybriden durch eine Kreuzbefruchtung zwischen einem diploiden Gametophyten, entstanden aus einer Diplospore, und einem haploiden Gametophyten hervorgegangen sind. Diplosporen könnten auch zur Vermehrung der diploiden Hybriden mittels Sporen beitragen; allerdings sind sie bei Flachbärlappen noch nicht experimentell eindeutig nachgewiesen. Bisherige Untersuchungen dreier genetischer Marker (cp, RPB, LFY) sowie die Ergebnisse einer AFLP-Analyse legen jedoch eine überwiegende de-novo-Entstehung durch primäre Kreuzungsereignisse nahe.
Die drei Elternarten unterscheiden sich hinsichtlich ihrer genetischen Diversität erheblich. Während von D. alpinum mindestens zwei genetische Linien existieren, ist D. tristachyum offensichtlich wenig variabel. Die größte genetische Vielfalt weist D. complanatum auf, für das eine sexuelle Reproduktion durch flowzytometrische Untersuchungen der gametophytischen Generation nachgewiesen werden konnte. Auch die Hybriden sind genetisch nicht einheitlich, was für unabhängige Entstehungsereignisse spricht.
Die Vertreter der Gattung Diphasiastrum weisen einen ausgeprägten Pioniercharakter auf und können Lebens-räume mit frühen Sukzessionsstadien erfolgreich besiedeln. Hier bilden sie durch ihr klonales Wachstum flächig ausgedehnte Bestände (Klone) aus. Diese können, längerfristig geeignete Standortbedingungen vorausgesetzt, ein Alter von vielen Jahrzehnten bis zu mehreren Hundert Jahren erreichen. Mit ihren staubfeinen Sporen sind Flachbärlappe auch zur Besiedlung von Gebieten, die von bestehenden Vorkommen weiter entfernt sind, mittels Langstreckentransport durch die Luft befähigt.
Flachbärlappe sind obligate Dunkelkeimer mit sich über mehrere Jahre erstreckenden Entwicklungszyklen. Die heterotrophen unterirdisch lebenden Gametophyten benötigen für Ihre Entwicklung Mykorrhizapilze. Funde von Gametophyten des Alpen-Flachbärlapps boten die Möglichkeit, den assoziierten Mykorrhizapilz morphologisch und genetisch zu untersuchen. Dieser wurde als zur Sebacinales-Gruppe B (Agariomycota) zugehörig identifiziert. Diese Pilzgruppe ist auch als Mykorrhizapartner von Ericaceen (Heidekrautgewächse) bekannt. Da keine Hinweise auf eine Mykorrhizierung des sporophytischen Bärlapp-Gewebes gefunden wurden, ist die Beziehung zwischen Pilz und Bärlapp möglicherweise nicht symbiotischer sondern parasitischer Natur. Der mykoheterotrophe Bärlapp-Gametophyt würde in diesem Fall epiparasitisch auf Vertretern der Ericaceen leben. Dies würde die regelmäßige Vergesellschaftung von Flachbärlappen mit verschiedenen Heidekrautgewächsen erklären. Eine ericoide Mykorrhiza bei Bärlappen, bestehend aus einem Netzwerk zwischen Ericaceen, Mykorrhizapilzen und Bärlapp-Gametophyten, wurde zuvor nicht beobachtet.
Die aktuelle Verbreitung der Flachbärlappe ist in den meisten Landesteilen Deutschlands und auch in einigen anderen Regionen Mitteleuropas weitgehend bekannt. Ihre früheren Arealbilder sind hingegen erst für Teilgebiete geklärt, was auf ihre schwierige Bestimmbarkeit und der über Jahrzehnte in der botanischen Literatur bestehenden taxonomischen Verwirrung zurückzuführen ist. Die frühere Verbreitung konnte auf der Basis kritischer Herbarrevisionen bislang für Niedersachsen und Bremen, Nordrhein-Westfalen, Thüringen und Teilgebiete Hessens und Bayerns rekonstruiert werden.
Die standortökologischen Ansprüche der Flachbärlapp-Sippen sind für Deutschland und einige Regionen angrenzender Länder hingegen gut untersucht. Es werden Sandböden mit unterschiedlich hohen Lehm- und Tonanteilen besiedelt, die relativ humusreich sind und größere Skelettanteile aufweisen können. Die Böden sind trocken bis frisch, reagieren sehr stark bis stark sauer (pH-Werte zwischen 2,9 und 4,5) und sind nährstoffarm (Stickstoffgehalte im Mittel zwischen 0,12 % und 0,25 %). Hinsichtlich ihrer Lichtansprüche unterscheiden sich die Flachbärlapp-Taxa erheblich. D. complanatum, D. tristachyum und ihre Hybride D. x zeilleri besiedeln recht heterogene Wuchsorte und sind sowohl an halbschattigen als auch lichtreichen Standorten zu finden (relativer Lichtgenuss meist zwischen 20 % und 80 %). D. alpinum und seine Hybriden D. x issleri und D. x oellgaardii bevorzugen dagegen offene Wuchsorte mit einem relativen Lichtgenuss zwischen 80 % und 100 %.
Die allermeisten Vorkommen von Flachbärlappen sind in Mitteleuropa heute an Sekundärstandorten anthropogenen Ursprungs zu finden. Primärstandorte stellen außerhalb des Alpenraumes die große Ausnahme dar. Die Vergesellschaftung der Flachbärlappe ist gut dokumentiert. Neben verschiedenen von Nadelhölzern dominierten Wald- und Forstgesellschaften (Leucobryo-Pinetum, Cladonio-Pinetum, Vaccinio myrtilli-Piceetum) treten sie in verschiedenen Vegetationstypen des Offenlandes mit lückiger und kurzrasiger Struktur auf (Vaccinio-Callunetum, Genisto anglicae-Callunetum, Violion- und Nardion-Gesellschaften, Festuca nigrescens-Agrostis capillaris-Bestände).
Die Flachbärlappe sind seit Jahrzehnten von einem dramatischen Bestandsrückgang betroffen und werden daher in den meisten nationalen Roten Listen Mitteleuropas als stark gefährdet oder sogar als vom Aussterben bedroht geführt. Hauptgrund ist das fast vollständige Verschwinden ihrer ehemaligen Lebensräume durch Aufgabe traditioneller Nutzungsformen und Änderungen in der forstlichen Bewirtschaftung. Die zunehmende Eutrophierung durch die ständig intensiver werdende Landwirtschaft stellt einen sukzessionsbeschleunigenden Faktor dar und bedingt, dass die Verweildauer eines Bestandes an einem Sekundärstandort ohne pflegende Eingriffe mittlerweile auf maximal 10 bis 15 Jahre gesunken sein dürfte. Allerdings lassen sich die Bestände durch das regelmäßige manuelle Entfernen bzw. Eindämmen pflanzlicher Konkurrenten stützen und ihre Überlebensdauer damit deutlich erhöhen, wie Erfahrungen im Rahmen diverser Artenhilfsprogramme in verschiedenen Teilen Deutschlands gezeigt haben. Auch die Flachbärlapp-Hybriden bilden langlebige und flächig ausgedehnte Klone aus und können fernab einer oder sogar beider Elternarten auftreten. Unabhängig von ihrer noch ungeklärten generativen Reproduktionsfähigkeit verhalten sie sich wie unabhängige Arten und sollten daher naturschutzfachlich auch als solche bewertet werden.
Der starke Rückgang sowie eine hohe internationale Verantwortlichkeit Deutschlands für einige Diphasiastrum-Taxa, speziell für D. x issleri und D. x oellgaardii, zeigen die dringende Notwendigkeit für gezielte Artenhilfsprogramme für diese faszinierende Pflanzengruppe.
Peatlands are the most space-efficient terrestrial carbon sink on earth, storing more carbon than all other vegetation types in the world combined. The amount of carbon input into peatlands is determined by the primary production and decomposition of plants. The fragile relationship between these two processes is massively disturbed by intensive land use and the associated drainage of large peatland areas, releasing as much carbon dioxide annually as global air travel. Aiming for the substantial reduction of greenhouse gas emissions, rewetting measures have been initiated worldwide to protect and sustainably manage peatlands by restoring the waterlogged conditions required for peat formation. However, the increase in droughts across Europe adds another threat for peatlands by lowering water tables and affecting plant productivity, litter decomposition and phenology, which can reduce their potential for carbon storage.
Fens are minerotrophic peatlands that make up over a third of the peatland area in Europe. The growth and turnover of root biomass is particularly important for the formation and degradation of peat in fens; thus, a special focus should lie on root dynamics research. However, despite their pivotal role for peat formation, we still lack knowledge about root responses to environmental changes caused by rewetting or drought in fens. This thesis aims to advance our knowledge about root processes as well as their abiotic drivers in drained and rewetted fen peatlands of NE Germany, and how they may be affected by an extreme drought. For this purpose, destructive (i.e. in-growth cores, litter bags, soil coring) along with non-destructive measurements (i.e. minirhizotrons, NDVI) were used in situ in forested (alder forests) and graminoid-dominated (sedges and grasses) plant communities representative of the prevailing fen peatlands of Central Europe.
In this thesis, I investigate the environmental drivers of root growth (Chapters I-III), the annual production and decomposition (Chapter II), phenology and temporal dynamics of root growth (Chapters I and III), and the response of root biomass distribution and their functional traits to environmental changes linked to rewetting (Chapter IV). To understand the fundamental differences in productivity of plant communities on mineral and organic soils, above-and belowground phenology and their environmental drivers were compared among different temperate ecosystems (i.e. a beech forest, a forested peatland and two graminoid-dominated fen peatlands) in Central Europe (Chapter I). The study provides evidence that generalizations of aboveground to belowground production are not likely to reflect seasonal dynamics in temperate fen peatlands. Furthermore, the study shows that fine root production can be up to 10 times higher for peatland plant communities than for a beech forest on mineral soil, highlighting the importance of roots for contributing substantially to the formation of organic soils. By comparing annual productivity and decomposition between drained and rewetted fens, it is shown that rewetted fens maintained their productivity under the drought conditions experienced in Central Europe in the year 2018, leading to a higher carbon storage potential despite similar decomposition rates (Chapter II). A deeper understanding on the drivers of this high productivity in the rewetted sites is provided by the analysis of temporal dynamics of root growth and their potential abiotic drivers (Chapter III). Here, the important role of root phenology in the maintenance of productivity of rewetted fens under drought conditions is revealed, since higher root productivity in response to rewetting was driven by an extension of the growing season rather than through a higher growth rate (Chapter III). This thesis shows that rewetting can be beneficial for plant production under drought conditions, which is central to the maintenance of the carbon sink function of peatlands (Chapters II and III). Rewetting maintained high water tables, favouring a plant community adapted to water saturation and also to fluctuating environmental conditions, and thus a community able to cope with periodic water table drawdowns that might increase in the future. Contrarily, drainage caused water tables to constantly drop below rooting depth of plants that might be adapted to drier conditions, but not drought. To gain a deeper understanding of the changes that roots undergo with rewetting and their potential effects on soil carbon storage, a fourth study focuses on the changes in biomass distribution and functional traits of roots along the soil profile (Chapter IV). Together with root age determination the study indicates higher rates of carbon turnover in shallow soil layers and higher belowground carbon investments with rewetting compared to drainage in a forested peatland.
This thesis demonstrates that generalizations of phenological events from plant communities of mineral to organic soils, even though they face the same macroclimatic conditions, are misleading, as they are not subject of the same environmental controls (Chapter I). Rewetting of forest and graminoid-dominated fen peatlands supports their function as carbon sink by enhancing renewed carbon sequestration in form of root biomass (Chapters II-IV). Knowledge about root phenology is crucial to understand plant productivity of peatlands, one of the main drivers of organic matter accumulation (Chapter III). Even though roots are pivotal for mediating the input of carbon into the soil, their dynamics remain one of the least understood aspects of plant function. This thesis contributes to fill this knowledge gap by shedding light on root processes that contribute to the formation of peat and the complexity of the underlying abiotic drivers in rewetted and drained fens in face of a warmer and drier climate.
Species have to cope with climate change either by migration or by adaptation and acclimatisation. Especially for long-living tree species with a low seed dispersal capacity (e.g. European beech, hereafter called beech), the in situ responses through genetic adaptation and phenotypic plasticity play an important role for their persistence. Beech, the dominant climax tree species in Central Europe, shows a high drought sensitivity and its distribution range is expected to shift northwards. On the other hand, projected northward shifts need to be taken with caution, as some studies suggest a sensitivity of beech to frost events in winter and spring. However, studies on the growth performance of cold-marginal beech populations are still rare. Previous studies on beech populations found local adaptation to drought and phenotypic plasticity in fitness-related traits as well as phenological traits. However, studies on the regeneration of beech under natural conditions are yet missing, although germination and establishment of young trees are a very first selective bottleneck and are crucial for tree population persistence and for successful range shifts.
This PhD-thesis aimed to identify the potential of plasticity and local adaptation in the important early life-history traits germination, establishment after the 1st year, and survival after the 2nd year in a reciprocal transplantation experiment at 11 sites across and even beyond the distribution range of beech (Manuscript 1). Moreover, this thesis investigated the climate sensitivity and the adaptation potential of beech populations by conducting dendroecological studies along a large climatic gradient across the distribution range (Manuscript 2) and along a strong winter temperature gradient towards the cold distribution margin in Poland (Manuscript 3). In addition, the impact of local climatic singularities was studied in a local study at the southern margin (Manuscript 4).
Warm and dry conditions limited natural regeneration, which was indicated by very low survival of young trees, even though germination rates increased with increasing temperature (Manuscript 1). This was also the case in parts of the distribution centre due to the hot and dry conditions in 2018. Although the transplantation experiment revealed high plasticity in the early life-history traits, this plasticity might thus not buffer against climate change under dry conditions. Local adaptation was not detected for any of these traits along the climatic gradient. In contrast, the results of the dendroecological study across the gradient (Manuscript 2) hint towards an adaptation potential of adult trees to drought at the southern margin. Thus, adult trees seemed to be adapted to drought at the southern margin, whereas tree growth in the distribution centre was sensitive to drought. These results indicate that parts of the centre may become ecologically marginal with increasing drought frequency in times of climate change. Interestingly, Manuscript 4 shows that beech growth was positively influenced by frequent fog immersion at the southern distribution margin in north-eastern Spain. This study underlines the importance of local climatic singularities, as they may allow marginal populations to grow in climate refugia in an otherwise unfavourable climate.
At the cold distribution margin, the study in Manuscript 1 found a remarkably higher survival of young trees in Sweden than in Poland. Moreover, the dendroecological studies revealed that beech was hampered by both drought at the cold-dry margin (Manuscript 2) and by winter cold at the cold-wet margin in Poland (Manuscript 3). All these results highlight the importance to study climate sensitivity of adult trees and the response of early life-history traits at the cold margin with a more differentiated view comparing cold-dry against the cold-wet populations and growing conditions. However, the high plasticity of the early life-history traits may allow for an increasing germination rate with climate warming at the northern margin and may thus facilitate natural regeneration there. In contrast, the dendroecological studies suggest that adult trees at the cold distribution margin may suffer either from drought or from winter cold and that the risk for spring frost may increase. Thus, the often-predicted compensation of dry-marginal population decline by a northward range expansion should be discussed more critically.
In conclusion, my PhD thesis provides new knowledge about the potential of natural regeneration and about climate sensitivity of adult trees across the distribution range of beech. Moreover, it underlines the importance to study both the young tree stages as well as adult trees to assess the performance and vulnerability of tree species under climate change, as both showed differences in their response to changing environmental conditions.
Der rundblättrige Sonnentau (Drosera rotundifolia L.) ist typisch für nährstoffarme Hochmoore und nimmt eine besondere Rolle im Moor-Ökosystem ein. Die Pflanzenart gilt in vielen europäischen Ländern als gefährdet bzw. stark gefährdet. Ihre Gefährdung lässt sich auf drei Ursachen zurückführen:
1) Seit Jahrzehnten führt die Bewirtschaftung der europäischen Moore und die damit einhergehende Entwässerung und Düngung zu einem deutlichen Rückgang der von Drosera-Arten bevorzugten oligotrophen, nassen und sauren Standorte.
2) Bereits im Mittelalter waren Drosera-Arten als Heilpflanzen bekannt und wurden hauptsächlich zur Behandlung von Atemwegserkrankungen (Asthma, Bronchitis, Keuchhusten etc.) eingesetzt.
3) Obwohl seit den 1920er Jahren bereits immer wieder Kultivierungsversuche mit Drosera-Arten durchgeführt wurden, konnte bisher keine Methode für den großflächigen Anbau von Sonnentau realisiert werden, um die von der Pharmaindustrie benötigten Mengen des Drosera-Rohstoffs zu produzieren. Daher werden bis heute europäische und nicht europäische Drosera-Arten immer noch in großen Mengen in natürlichen Mooren gesammelt.
Die zunehmende Zerstörung der natürlichen Moore und die Sammlung für arzneiliche Zwecke stellen zusammen eine ernsthafte Bedrohung für den Erhalt von D. rotundifolia dar. Die Torfmooskultivierungsflächen in Deutschland sind in vieler Hinsicht vergleichbar mit intakten Hochmooren. Das nährstoffarme Milieu der kultivierten Torfmoose dient als Lebensraum für heimische Drosera-Arten, wie Drosera rotundifolia L. und Drosera intermedia Hayne. Daher bieten diese Kulturflächen eine neue Alternative für den Anbau von Drosera-Arten.
In vier Studien wurde die Eignung von Torfmoosrasen für den Drosera-Anbau untersucht, mit Schwerpunkt auf den Anbau von Drosera rotundifolia auf Torfmoos- kultivierungsflächen. In der ersten Studie wurde das Wissen über die Morphologie, Verbreitung, Ökologie, Reproduktion, Nutzung, den Schutz und den Anbau von D. rotundifolia erstmals zusammenfassend diskutiert, um eine wissenschaftliche Grundlage für einen erfolgreichen Anbau auf Torfmoosrasen zu schaffen. Basierend auf diesen Kenntnissen konzentriert sich die zweite Studie auf die Keimfähigkeit von D. rotundifolia und die Überlebensrate von jungen Drosera-Pflanzen auf Torfmoosrasen unter natürlichen, naturnahen und künstlichen Bedingungen. Die dritte Studie fokussiert auf den Gehalt pharmakologisch wirksamer Inhaltsstoffe angebauter und „wild wachsender“ D. rotundifolia- sowie D. intermedia-Pflanzen auf Torfmooskultivierungsflächen. Die vierte Studie untersucht die Biomasseproduktivität und den Ertrag, d. h. den Biomasseanteil der geerntet wird, von beiden o. g. Drosera-Arten auf Torfmooskultivierungsflächen.
Die generierten Daten und Erkenntnisse der vier Studien wurden in vier wissenschaftlichen Artikeln zusammengefasst, wovon zwei bereits veröffentlicht und zwei eingereicht sind.
Die wichtigsten Ergebnisse dieser Studien sind die Folgenden:
I) Drosera rotundifolia ist sehr stark mit Sphagnum-dominierten Pflanzengemeinschaften verbunden, welche durch Entwässerung europaweit zurückgegangen bzw. verschwunden sind. Dadurch ist D. rotundifolia in den meisten europäischen Ländern eine seltene und geschützte Pflanzenart geworden.
II) Verschiedene Drosera-Arten, u. a. D. rotundifolia, D. intermedia, D. anglica und D. madagascariensis, werden immer noch von Pharmaunternehmen verwendet. Die Pflanzen werden in der freien Natur gesammelt, weil deren Anbau zeitaufwendig und (noch) nicht effizient ist. Daher ist die Entwicklung von Anbaumethoden erforderlich.
III) Die selbstentwickelte „Torf-Gefäß-Methode“ ergab sich als die meist geeignete Drosera-Anbau-Methode durch das spezielle Mikroklima des Sphagnum- Rasens, das konkurrenzarme Milieu und den permanent nassen Sphagnum- Torf in den Pflanzgefäßen.
IV) In den Feldversuchen wurden bei der Aussaat sehr niedrige Keimungsraten < 1 % registriert. Deshalb sind für den Anbau mit Aussaat große Mengen an Samen erforderlich.
V) Die Entfernung von Gefäßpflanzen zeigte im ersten Jahr eine positive Korrelation mit der Anzahl der Drosera-Keimlinge und führte im zweiten Jahr zu einer höheren Anzahl überlebender Drosera-Pflanzen.
VI) Auf Torfmooskultivierungsflächen wachsende Drosera-rotundifolia-Pflanzen wiesen eine 7- bis 8-mal höhere Konzentration von 7-Methyljuglon auf als D. madagascariensis, die hauptsächlich für ‘Droserae herba’ verwendet wird.
VII) Für Drosera rotundifolia gab es bezüglich der Tageszeit keine signifikanten Unterschiede in den Konzentrationen bioaktiver Inhaltsstoffe. Dies bedeutet, sie kann ganztägig zwischen 7 und 16 Uhr gesammelt werden. Die höchsten Konzentrationen bioaktiver Inhaltsstoffe wurden für D. rotundifolia und D. intermedia bei 13 bis 24 Monate alten blühenden Pflanzen festgestellt
VIII) Im Vergleich zu natürlichen Mooren Mittel- und Nordeuropas, zeigte D. rotundifolia auf den Torfmooskultivierungsflächen eine 3-34 Mal höhere Biomasseproduktivität (275 kg ha-1 a-1) und einen 2-21 Mal höheren Ertrag (214 kg ha-1 a-1).
IX) Der höchste Ertrag von D. rotundifolia und D. intermedia wurde im Juli und August dokumentiert. In diesen Monaten erreichen die Pflanzen ihr höchstes Gewicht. Auf Torfmooskultivierungsflächen erreichte D. rotundifolia einen viermal höheren Ertrag als D. intermedia. Deshalb ist D. rotundifolia für den Anbau zu bevorzugen.
X) Für eine langfristige nachhaltige Produktion von Drosera wird die Ernte von mindestens 12 Monate alten Pflanzen empfohlen.
Tree growth in northern and upper treeline ecotones of the circumpolar boreal forest is
generally limited by temperature, i.e., trees grow generally more under warm, and less under
cold climatic conditions. Based on the assumption that this relationship between tree growth
and climate is linear and stable through time, dendroclimatologists use tree rings as natural
archives to reconstruct past temperature conditions. Such tree-ring based reconstructions,
together with other natural archives (e.g., ice cores and pollen), constitute our understanding of
past climatic conditions that reach beyond modern instrumental records.
However, a steadily increasing amount of studies reports a recent reduction or loss of the
summer temperature signal for several species and sites of the boreal forest. Such a reduction
of temperature sensitivity results in temporally unstable climate-tree growth relationships,
which challenges the work of dendroclimatologists by potentially leading to miscalibrations of
past climatic conditions. On the upside, this shift in the trees’ climate sensitivity might point to
a shift in tree growth-limiting factors and thus serve as an early indicator of climate change
impacts. There is evidence that this recent reduction in temperature sensitivity might be caused
by the observed strong temperature increase at high latitudes, and thus temperature-induced
drought stress. Other potential drivers and amplifiers of this phenomenon are differing microsite
conditions (dry vs. wet soils) and factors inherent to trees, like genetic properties or age
effects.
In this PhD thesis, I systematically assessed the effects of frequently discussed drivers of
unstable climate-tree growth relationships (climate change, micro-site effects, genetical
predisposition) on two representative species of the boreal forest, white spruce in North
America and Scots pine in Eurasia, across various temporal and spatial scales. I used classical
(tree-ring width) and more novel (wood density, quantitative wood anatomy)
dendrochronological proxies to unravel the effects from annual to sub-monthly resolution.
More precisely, in chapter I, white spruce clones were compared to non-clones at two treeline
sites in Alaska to test whether their growth patterns differ, and whether white spruce clones are
generally suitable for dendroclimatic assessments. Clonal reproduction is frequent at treeline
due to harsh conditions, but might lead to competition among individuals due to the close
proximity among each other, which in turn might obscure their climatic signal. Second, I tested
the effect of warmer and drier climatic conditions on the summer temperature signal of Scots
pine in Eurasia (chapter II) and on the growing season moisture signal of white spruce in North
America (chapter III), respectively. Temperature-induced drought stress is expected to be the
most important driver of unstable climate-growth relationships in the boreal forest. I included
several sites across latitudinal (50-150 km) and longitudinal (1,000-2,200 km) gradients to
cover large parts of the species’ distribution ranges. Since Scots pine covers a wide range of
ecological habitats, I additionally tested the effect of dry and wet micro-site conditions on the
summer temperature signal of Scots pine in chapter II. Finally, in chapter IV, a systematic
literature review was carried out in order to investigate the distribution of unstable climategrowth
relationships in global tree-ring studies, and the usage of such series in climate
reconstructions. Furthermore, the scientific impact of these potentially inaccurate climate
reconstructions was assessed.
In this PhD project, warmer and drier climatic conditions led to temporally unstable climate
signals in both Scots pine (chapter II) and white spruce (chapter III), as expected. Unstable
climate-growth relationships were found for all tested tree-ring proxies and at all sites in North
America, and at most sites in Eurasia. Micro-site effects (chapter II) and clonal growth
(chapter I) had no significant effect on the climate sensitivity and high-frequency variability
of the tested species, but affected absolute growth. The review (chapter IV) revealed that the
phenomenon of unstable climate-growth relationships is globally widespread, and occurs
independent of tree species, geographic location, and tree-ring and climate proxies. While
reconstructions inferred from these unstable relationships are frequent and respective papers
have a high impact, the tree-ring community seems to increasingly recognize the challenge of
unstable climate-growth relationships.
With these findings, this PhD project helped to shed more light on the frequency, underlying
drivers, and the impact of unstable climate-growth relationships in boreal forest trees, as well
as underlying reaction processes in trees. Above all, this PhD project suggests that the loss of
climate sensitivity is caused by a change of growth limiting factors: temperature limitation
seems to be suspended in warmer and drier years for Scots pine in Eurasia, and moisture
limitation first arises under warm/dry conditions for white spruce in North America. Due to
plastic growth responses in trees, the general assumption in dendroclimatology – that climategrowth
relationships are stable through time – seems to be incompatible with the principle of
limiting factors (one factors is always most growth limiting).
To improve the validity of future climate reconstructions, statistical approaches considering
synchronously or changing climatic limiting factors need to be promoted, along with attempts
to select the best responding trees from a dataset. Furthermore, a better understanding of nonclimatic
factors potentially affecting tree growth (e.g., age, disturbance, soil parameters) is
needed. A growth reduction of mature and dominant white spruce trees sampled in this PhD
project seems likely under future warming conditions, with series of wood cells being valuable
early indicators of climate change effects in white spruce. However, inferences cannot be
extended to the entire stand due to the applied sample design. Projected climate warming will
probably lead to a further reduction of the summer temperature signal in trees of the northern
boreal forest, while wider consequences for forest growth and productivity are unclear.