TY - JOUR A1 - Heinrichs, Steffi A1 - Ammer, Christian A1 - Mund, Martina A1 - Boch, Steffen A1 - Budde, Sabine A1 - Fischer, Markus A1 - Mueller, Joerg A1 - Schoening, Ingo A1 - Schulze, Ernst-Detlef A1 - Schmidt, Wolfgang A1 - Weckesser, Martin A1 - Schall, Peter T1 - Landscape-Scale Mixtures of Tree Species are More Effective than Stand-Scale Mixtures for Biodiversity of Vascular Plants, Bryophytes and Lichens JF - Forests N2 - Tree species diversity can positively affect the multifunctionality of forests. This is why conifer monocultures of Scots pine and Norway spruce, widely promoted in Central Europe since the 18th and 19th century, are currently converted into mixed stands with naturally dominant European beech. Biodiversity is expected to benefit from these mixtures compared to pure conifer stands due to increased abiotic and biotic resource heterogeneity. Evidence for this assumption is, however, largely lacking. Here, we investigated the diversity of vascular plants, bryophytes and lichens at the plot (alpha diversity) and at the landscape (gamma diversity) level in pure and mixed stands of European beech and conifer species (Scots pine, Norway spruce, Douglas fir) in four regions in Germany. We aimed to identify compositions of pure and mixed stands in a hypothetical forest landscape that can optimize gamma diversity of vascular plants, bryophytes and lichens within regions. Results show that gamma diversity of the investigated groups is highest when a landscape comprises different pure stands rather than tree species mixtures at the stand scale. Species mainly associated with conifers rely on light regimes that are only provided in pure conifer forests, whereas mixtures of beech and conifers are more similar to beech stands. Combining pure beech and pure conifer stands at the landscape scale can increase landscape level biodiversity and conserve species assemblages of both stand types, while landscapes solely composed of stand scale tree species mixtures could lead to a biodiversity reduction of a combination of investigated groups of 7 up to 20%. KW - Fagus sylvatica KW - Pinus sylvestris KW - Picea abies KW - Pseudotsuga menziesii KW - forest management KW - tree species diversity KW - forest conversion KW - gamma diversity KW - landscape scale KW - Biodiversity Exploratories Y1 - 2019 U6 - https://doi.org/10.3390/f10010073 SN - 1999-4907 VL - 10 IS - 1 PB - MDPI CY - Basel ER - TY - JOUR A1 - Leuschner, Christoph A1 - Wulf, Monika A1 - Bäuchler, Patricia A1 - Hertel, Dietrich T1 - Soil C and nutrient stores under Scots pine afforestations compared to ancient beech forests in the German Pleistocene - the role of tree species and forest history JF - Forest ecology and management N2 - In the diluvial lowlands of northern Germany, the Netherlands and northern Poland, an estimated similar to 5 Mio ha of Scots pine plantations (Pinus sylvestris) has been established on sandy soil in the last 250 years replacing the former temperate broad-leaved forests after extended periods of cultivation in the Middle Ages. We examined the effect of variable stand continuity of pine plantations (recent vs. ancient: 51-128 vs. >230 years) on the soil organic carbon (SOC) store and soil nutrient capital in comparison to ancient beech forests (>230 years of continuity) which represent the potential natural forest vegetation. Recent and ancient pine stands had c. 75% larger organic layer C stores than ancient beech forests, while the total C stock in the soil (organic layer and mineral soil to 100 cm) was similar to 25% larger in the beech forests due to higher C concentrations in 0-50 cm depth of the mineral soil. The soil stores of N-tot were similar to 50% and the exchangeable Ca, K and Mg pools about three times larger under beech than under the pine stands. Resin-exchangeable P was enriched in the soils under ancient pine stands probably due to manuring in the past. After clear-cut and long cultivation, it may take >230 years of forest presence to restore the greatly reduced mineral soil C and N pools. The C and N sequestration potential of the soils appeared to be particularly small under pine indicating a pronounced tree species (pine vs. beech) effect on soil C and N dynamics. We conclude that, in the face of rising greenhouse gas emissions, the limited soil C and nutrient storage potential of Scots pine plantations on sandy soils needs consideration when selecting suitable tree species for future forestry. (C) 2013 Elsevier B.V. All rights reserved. KW - Sandy soil KW - Pinus sylvestris KW - Fagus sylvatica KW - Forest continuity KW - Historic land use KW - Nitrogen Y1 - 2013 U6 - https://doi.org/10.1016/j.foreco.2013.08.043 SN - 0378-1127 SN - 1872-7042 VL - 310 IS - 6 SP - 405 EP - 415 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Liang, Wei A1 - Heinrich, Ingo A1 - Simard, Sonia A1 - Helle, Gerhard A1 - Linan, Isabel Dorado A1 - Heinken, Thilo T1 - Climate signals derived from cell anatomy of Scots pine in NE Germany JF - Tree physiology N2 - Tree-ring chronologies of Pinus sylvestris L. from latitudinal and altitudinal limits of the species distribution have been widely used for climate reconstructions, but there are many sites within the temperate climate zone, as is the case in northeastern Germany, at which there is little evidence of a clear climate signal in the chronologies. In this study, we developed long chronologies of several cell structure variables (e. g., average lumen area and cell wall thickness) from P. sylvestris growing in northeastern Germany and investigated the influence of climate on ring widths and cell structure variables. We found significant correlations between cell structure variables and temperature, and between tree-ring width and relative humidity and vapor pressure, respectively, enabling the development of robust reconstructions from temperate sites that have not yet been realized. Moreover, it has been shown that it may not be necessary to detrend chronologies of cell structure variables and thus low-frequency climate signals may be retrieved from longer cell structure chronologies. The relatively extensive resource of archaeological material of P. sylvestris covering approximately the last millennium may now be useful for climate reconstructions in northeastern Germany and other sites in the temperate climate zone. KW - cell structure KW - dendroclimatology KW - Pinus sylvestris KW - quantitative wood anatomy KW - tree rings Y1 - 2013 U6 - https://doi.org/10.1093/treephys/tpt059 SN - 0829-318X SN - 1758-4469 VL - 33 IS - 8 SP - 833 EP - 844 PB - Oxford Univ. Press CY - Oxford ER - TY - GEN A1 - Heinken, Thilo T1 - Die natürlichen Kiefernstandorte Deutschlands und ihre Gefährdung T1 - Natural Scots pine forests in Germany : habitats, distribution, and threat N2 - Natürliche Standorte der Waldkiefer gibt es in Deutschland nur kleinflächig. Während Kiefernforste anstelle natürlicher Laubwälder heute oft landschaftsprägend sind, bildet die konkurrenzschwache und lichtbedürftige Kiefer ausschließlich auf extrem trockenen oder nassen, nährstoffarmen Standorten naturnahe Schlusswaldgesellschaften. Regionale Schwerpunkte liegen in subkontinentalen Regionen wie dem nordostdeutschen Tiefland und Bayern, ein „natürliches Kiefernareal" lässt sich aber kaum abgrenzen. An der Trockengrenze des Waldes finden sich auf Kalk- und Dolomitgesteinen artenreiche Karbonat-Trockenkiefernwälder mit Elementen der alpinen Rasen und Kalkmagerrasen in der Bodenvegetation. Diese Wälder besiedeln steile, südexponierte Felsen und morphodynamisch aktive Bereiche wie Rutschhänge und FlussSchotterböden im Umkreis der Alpen, kommen aber auch in den Mittelgebirgen vor. Ihr Gegenstück auf sauren Standorten sind die Sand- und Silikat-Kiefernwälder der Quarzsande und Sandstein-Verwitterungsböden, deren Bodenvegetation durch Zwergsträucher, Moose und Strauchflechten geprägt ist. Hier siedelt die Kiefer in den Tieflagen besonders auf Binnendünen und Sandern, aber auch auf Küstendünen der Ostsee, in den Mittelgebirgen z. B. auf den Sandsteinriffen der Sächsischen Schweiz. Der dritte Wuchsbereich natürlicher Kiefernwälder sind saure, nährstoffarme Moore, die ganz überwiegend von Regenwasser gespeist werden. Auch die Kiefern-Moorwälder sind in Nordostdeutschland und Bayern am häufigsten. Von diesen Standorten ausgehend, wo ihr Platz kaum von anderen Baumarten streitig gemacht wird, tritt die Waldkiefer immer wieder als Pionier auf weniger extremen Standorten auf. In der Naturlandschaft kam dies etwa nach Waldbränden oder Stürmen vor, doch der Mensch förderte die Kiefer durch Auflichtung der Wälder, Waldweide und Streunutzung stark. Auch die damit verbundene Nährstoffverarmung macht eine exakte Abgrenzung natürlicher Kiefernstandorte unmöglich. Die schlechtwüchsigen und forstwirtschaftlich nicht interessanten, ästhetisch aber sehr ansprechenden natürlichen Kiefernbestände sind heute vor allem durch Stickstoff-Immissionen gefährdet. Trotz ihrer oft kargen Erscheinung besitzen sie einen hohen Wert für die Biodiversität und den Artenschutz. Neben bodenbewohnenden Flechten und regionalen Relikt-Endemiten ist vor allem die in den letzten Jahrzehnten zunehmend gefährdete Vielfalt an Mykorrhiza-Pilzen hervorzuheben, die der Kiefer das Leben auf extrem nährstoffarmen Standorten überhaupt ermöglichen. Abschließend werden mögliche Schutz- bzw. Regenerationsmaßnahmen wie das Abplaggen flechtenreicher Kiefernstandorte vorgestellt. N2 - Only small areas of natural Scots pine (Pinus sylvestris) habitat occur in Germany. Today pine plantations instead of natural deciduous forests often dominate the landscape. Yet, due to the competitive weakness and light demands of Scots pine, near-natural Scots pine climax communities are only found on extremely dry or wet, nutrient-poor sites, primarily in subcontinental regions of the north-eastern German lowlands and Bavaria. However, the "natural distribution range" of Scots pine is difficult to define. Species-rich, dry Scots pine forests, with alpine and calcareous grassland species in the ground vegetation, are found at the aridity limit of forests on sites with carbonate rich soils developed from limestone and dolomite parent material. These forests occur on steep south-facing slopes, on morphodynamically active areas such as landslides and coarse river gravel beds in and near the Alps, and also in the low mountain ranges. Scots pine forests are also found on acidic sites, on quartz sands and soils overlying weathered silicate rocks with an understorey dominated by dwarf shrubs, bryophytes and fruticose lichens. These forests are present in the lowlands, particularly on inland dunes and glacifluvial deposits, but also on coastal dunes around the Baltic Sea and in the low mountain ranges, for example on the sandstone cliffs in the Elbe Sandstone Mountains. Acidic, oligo-trophic bogs, mainly supplied by rainwater, comprise the third natural Scots pine forest habitat. These Scots pine bog forests occur most frequently in north-eastern Germany and in Bavaria. Coming from these habitats, where virtually no other tree species grows, Scots pine is found again and again as a pioneer on less extreme sites. In the natural landscape, it occurs mainly after forest fires and storms. Yet humans promote Scots pine by thinning forests, creating woodland pasture and removing litter. The nutrient depletion associated with these practices makes an exact delimitation of natural Scots pine habitats unfeasible. Natural pine forest stands, which, although attractive and appealing, grow poorly and are of little interest for forestry, are endangered mainly by anthropo-genic nitrogen depositions. Despite their meagre appearance, these forests are important for biodiversity and species conservation. In addition to terricolous lichens and regional relic endemic plant species, the diversity of mycorrhiza fungi, which enable Scots pine to exist on these nutrient-poor sites, increasingly is becoming endangered. Finally, possible conservation and regeneration practices, such as manually cutting sods in lichen-rich Scots pine forests, are presented. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - paper 153 KW - Naturschutz KW - Phytodiversität KW - Pinus sylvestris KW - Standort KW - Walddynamik KW - nature conservation KW - phytodiversity KW - Pinus sylvestris KW - site conditions KW - forest dynamics Y1 - 2008 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-46506 ER -