TY - JOUR A1 - Scharf, Jan A1 - Becker, Michael A1 - Stallasch, Sophie E. A1 - Neumann, Marko A1 - Maaz, Kai T1 - Primary and secondary effects of social background across secondary education T1 - Primäre und sekundäre Herkunftseffekte über den Verlauf der Sekundarstufe BT - eine Dekomposition an drei Bildungsübergängen BT - decomposing effects at three educational transitions JF - Zeitschrift für Erziehungswissenschaft N2 - Secondary education is characterised by a sequence of transitions that are linked to educational inequality. Regarding social background effects, inequalities relate to disparities in educational achievement (primary effects) and educational decisions (secondary effects). In the present study, both primary and secondary effects are analysed based on an entire student cohort in the Hamburg school system (KESS study) across the course of secondary education, i.e. from entering secondary school to aiming for higher education. The KHB method is applied in order to decompose the effects, including transitions to upper secondary education. In line with previous research, total social background effects decrease across educational trajectories. No clear pattern emerges concerning an assumed increase in the relative importance of secondary effects. Primary effects operationalised by school grades are slightly predominant in the transition to lower secondary education, and nearly the same ratio is found for the transition to upper secondary education. However, regarding the aim to enter higher education, the relative importance of secondary effects is more clearly discernible. N2 - Die Sekundarstufe ist gekennzeichnet durch eine Sequenz von Übergängen, an denen Ungleichheiten durch Leistungsdisparitäten (primäre Effekte) und Bildungsentscheidungen (sekundäre Effekte) nach sozialer Herkunft relevant werden. Diese Herkunftseffekte werden mit dem vorliegenden Beitrag erstmals anhand von Daten einer vollständigen Schülerkohorte (Hamburger KESS-Studie) über den gesamten Verlauf der Sekundarstufe vom Übergang ins Gymnasium bis zur Studienintention analysiert. Eine Dekomposition und Quantifizierung primärer und sekundärer Effekte mit der KHB-Methode erfolgt dabei erstmals auch für den Eintritt in die Oberstufe. Abnehmende absolute Herkunftseffekte über den Bildungsverlauf, auf die bisherige Befunde verschiedener Stichproben verweisen, können mit dieser Studie zum Teil bestätigt werden. Zum vermuteten relativen Bedeutungszuwachs sekundärer Effekte zeigen die Ergebnisse kein eindeutiges Muster: Beim Wechsel ins Gymnasium überwiegen primäre Effekte leicht, wenn Noten als Leistungsindikator verwendet werden. Beim Eintritt in die Oberstufe bleibt die Relation nahezu unverändert. Erst bei der Studienintention fällt die relative Bedeutung sekundärer Effekte größer aus. KW - Complete survey KW - Decomposition KW - Educational transitions KW - Primary and KW - secondary effects KW - Social inequality KW - Bildungsübergänge KW - primäre und sekundäre Herkunftseffekte KW - Effektdekomposition KW - Vollerhebung KW - soziale Ungleichheit Y1 - 2020 U6 - https://doi.org/10.1007/s11618-020-00981-7 SN - 1434-663X SN - 1862-5215 VL - 23 IS - 6 SP - 1251 EP - 1282 PB - Springer CY - Wiesbaden ER - TY - JOUR A1 - Maes, Sybryn L. A1 - Blondeel, Haben A1 - Perring, Michael P. A1 - Depauw, Leen A1 - Brumelis, Guntis A1 - Brunet, Jörg A1 - Decocq, Guillaume A1 - den Ouden, Jan A1 - Haerdtle, Werner A1 - Hedl, Radim A1 - Heinken, Thilo A1 - Heinrichs, Steffi A1 - Jaroszewicz, Bogdan A1 - Kirby, Keith J. A1 - Kopecky, Martin A1 - Malis, Frantisek A1 - Wulf, Monika A1 - Verheyen, Kris T1 - Litter quality, land-use history, and nitrogen deposition effects on topsoil conditions across European temperate deciduous forests JF - Forest ecology and management N2 - Topsoil conditions in temperate forests are influenced by several soil-forming factors, such as canopy composition (e.g. through litter quality), land-use history, atmospheric deposition, and the parent material. Many studies have evaluated the effects of single factors on physicochemical topsoil conditions, but few have assessed the simultaneous effects of multiple drivers. Here, we evaluate the combined effects of litter quality, land-use history (past land cover as well as past forest management), and atmospheric deposition on several physicochemical topsoil conditions of European temperate deciduous forest soils: bulk density, proportion of exchangeable base cations, carbon/nitrogen-ratio (C/N), litter mass, bio-available and total phosphorus, pH(KCI)and soil organic matter. We collected mineral soil and litter layer samples, and measured site characteristics for 190 20 x 20 m European mixed forest plots across gradients of litter quality (derived from the canopy species composition) and atmospheric deposition, and for different categories of past land cover and past forest management. We accounted for the effects of parent material on topsoil conditions by clustering our plots into three soil type groups based on texture and carbonate concentration. We found that litter quality was a stronger driver of topsoil conditions compared to land-use history or atmospheric deposition, while the soil type also affected several topsoil conditions here. Plots with higher litter quality had soils with a higher proportion of exchangeable base cations, and total phosphorus, and lower C/N-ratios and litter mass. Furthermore, the observed litter quality effects on the topsoil were independent from the regional nitrogen deposition or the soil type, although the soil type likely (co)-determined canopy composition and thus litter quality to some extent in the investigated plots. Litter quality effects on topsoil phosphorus concentrations did interact with past land cover, highlighting the need to consider land-use history when evaluating canopy effects on soil conditions. We conclude that forest managers can use the canopy composition as an important tool for influencing topsoil conditions, although soil type remains an important factor to consider. KW - Soil fertility KW - Ancient forest KW - Post-agricultural forest KW - Coppice KW - High forest KW - pH KW - Phosphorus KW - Base cations KW - Nutrient cycling KW - Decomposition Y1 - 2019 U6 - https://doi.org/10.1016/j.foreco.2018.10.056 SN - 0378-1127 SN - 1872-7042 VL - 433 SP - 405 EP - 418 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Wang, Xinxin A1 - Huang, Xianyu A1 - Sachse, Dirk A1 - Hu, Yu A1 - Xue, Jiantao A1 - Meyers, Philip A. T1 - Comparisons of lipid molecular and carbon isotopic compositions in two particle-size fractions from surface peat and their implications for lipid preservation JF - Environmental earth sciences N2 - Knowledge of the possible impacts of early diagenesis on lipid biomarkers in geologic settings is important for robust applications of lipid proxies for paleoclimate reconstructions. In this study, molecular distributions and carbon isotopic compositions of lipids were compared in two particle-size fractions (<0.3 mm and >0.3 mm) of twelve surface peat samples collected from Dajiuhu peatland, central China. The average chain length (ACL) values of long-chain n-alkanes, n-fatty alcohols, n-fatty acids and n-alkan-2-ones show no significant differences between the finer and coarser fractions. In contrast, the carbon preference index values of long-chain n-alkanes, n-fatty alcohols and n-alkan-2-ones have relatively smaller values in the finer fractions than in the coarser ones. Stanols were also more abundant in the finer fractions. In addition, the delta C-13 values of odd-numbered n-alkanes (C-23-C-33) were generally less negative in the finer fractions. Our results indicate that (1) the finer fractions probably experienced stronger degradation than the coarser fractions; (2) the less negative delta(CC)-C-13 values of odd-numbered n-alkanes (C-23-C-33) in the finer fractions were largely a result of greater heterotrophic reworking during degradation; (3) ACL values of long-chain n-alkyl lipids (n-alkanes, n-fatty alcohols and n-fatty acids, n-alkan-2-ones) appear to be reliable proxies to trace lipid sources and their associated paleoenvironmental signals in peat deposits. KW - Peat KW - Lipids KW - Compound-specific carbon isotope KW - Particle-size fractions KW - Decomposition Y1 - 2016 U6 - https://doi.org/10.1007/s12665-016-5960-3 SN - 1866-6280 SN - 1866-6299 VL - 75 SP - 375 EP - 385 PB - Springer CY - New York ER - TY - JOUR A1 - Solly, Emily F. A1 - Schöning, Ingo A1 - Boch, Steffen A1 - Kandeler, Ellen A1 - Marhan, Sven A1 - Michalzik, Beate A1 - Müller, Jörg A1 - Zscheischler, Jakob A1 - Trumbore, Susan E. A1 - Schrumpf, Marion T1 - Factors controlling decomposition rates of fine root litter in temperate forests and grasslands JF - Plant and soil N2 - Fine root decomposition contributes significantly to element cycling in terrestrial ecosystems. However, studies on root decomposition rates and on the factors that potentially influence them are fewer than those on leaf litter decomposition. To study the effects of region and land use intensity on fine root decomposition, we established a large scale study in three German regions with different climate regimes and soil properties. Methods In 150 forest and 150 grassland sites we deployed litterbags (100 mu m mesh size) with standardized litter consisting of fine roots from European beech in forests and from a lowland mesophilous hay meadow in grasslands. In the central study region, we compared decomposition rates of this standardized litter with root litter collected on-site to separate the effect of litter quality from environmental factors. Standardized herbaceous roots in grassland soils decomposed on average significantly faster (24 +/- 6 % mass loss after 12 months, mean +/- SD) than beech roots in forest soils (12 +/- 4 %; p < 0.001). Fine root decomposition varied among the three study regions. Land use intensity, in particular N addition, decreased fine root decomposition in grasslands. The initial lignin:N ratio explained 15 % of the variance in grasslands and 11 % in forests. Soil moisture, soil temperature, and C:N ratios of soils together explained 34 % of the variance of the fine root mass loss in grasslands, and 24 % in forests. Grasslands, which have higher fine root biomass and root turnover compared to forests, also have higher rates of root decomposition. Our results further show that at the regional scale fine root decomposition is influenced by environmental variables such as soil moisture, soil temperature and soil nutrient content. Additional variation is explained by root litter quality. KW - Fine roots KW - Decomposition KW - Land use intensity KW - Lignin: N ratio KW - Temperate ecosystems Y1 - 2014 U6 - https://doi.org/10.1007/s11104-014-2151-4 SN - 0032-079X SN - 1573-5036 VL - 382 IS - 1-2 SP - 203 EP - 218 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Birkhofer, Klaus A1 - Diekoetter, Tim A1 - Boch, Steffen A1 - Fischer, Markus A1 - Müller, Jörg A1 - Socher, Stephanie A1 - Wolters, Volkmar T1 - Soil fauna feeding activity in temperate grassland soils increases with legume and grass species richness JF - Soil biology & biochemistry N2 - Edaphic fauna contributes to important ecosystem functions in grassland soils such as decomposition and nutrient mineralization. Since this functional role is likely to be altered by global change and associated shifts in plant communities, a thorough understanding of large scale drivers on below-ground processes independent of regional differences in soil type or climate is essential. We investigated the relationship between abiotic (soil properties, management practices) and biotic (plant functional group composition, vegetation characteristics, soil fauna abundance) predictors and feeding activity of soil fauna after accounting for sample year and study region. Our study was carried out over a period of two consecutive years in 92 agricultural grasslands in three regions of Germany, spanning a latitudinal gradient of more than 500 km. A structural equation model suggests that feeding activity of soil fauna as measured by the bait-lamina test was positively related to legume and grass species richness in both years. Most probably, a diverse vegetation promotes feeding activity of soil fauna via alterations of both microclimate and resource availability. Feeding activity of soil fauna also increased with earthworm biomass via a pathway over Collembola abundance. The effect of earthworms on the feeding activity in soil may be attributed to their important role as ecosystem engineers. As no additional effects of agricultural management such as fertilization, livestock density or number of cuts on bait consumption were observed, our results suggest that the positive effect of legume and grass species richness on the feeding activity in soil fauna is a general one that will not be overruled by regional differences in management or environmental conditions. We thus suggest that agri-environment schemes aiming at the protection of belowground activity and associated ecosystem functions in temperate grasslands may generally focus on maintaining plant diversity, especially with regard to the potential effects of climate change on future vegetation structure. KW - Above-belowground interactions KW - Bait lamina KW - Biodiversity ecosystem function research KW - Decomposition KW - Plant functional groups KW - Soil fauna KW - Spatial scale Y1 - 2011 U6 - https://doi.org/10.1016/j.soilbio.2011.07.008 SN - 0038-0717 VL - 43 IS - 10 SP - 2200 EP - 2207 PB - Elsevier CY - Oxford ER -