Direct and indirect associations between plant species richness and productivity in grasslands: regional differences preclude simple generalization of productivity-biodiversity relationships

Plant species richness of permanent grasslands has often been found to be significantly associated with productivity. Concentrations of nutrients in biomass can give further insight into these productivity- plant species richness relationships, e.g. by reflecting land use or soil characteristics. However, the consistency of such relationships across different regions has rarely been taken into account, which might significantly compromise our potential for generalization. We recorded plant species richness and measured above-ground biomass and concentrations of nutrients in biomass in 295 grasslands in three regions in Germany that differ in soil and climatic conditions. Structural equation modelling revealed that nutrient concentrations were mostly indirectly associated with plant species richness via biomass production. However, negative associations between the concentrations of different nutrients and biomass and plant species richness differed considerably among regions. While in two regions, more than 40% of the variation in plant species richness could be attributed to variation in biomass, K, P, and to some degree also N concentrations, in the third region only 15% of the variation could be explained in this way. Generally, highest plant species richness was recorded in grasslands where N and P were co-limiting plant growth, in contrast to N or K (co-) limitation. But again, this pattern was not recorded in the third region. While for two regions land-use intensity and especially the application of fertilizers are suggested to be the main drivers causing the observed negative associations with productivity, in the third region the little variance accounted for, low species richness and weak relationships implied that former intensive grassland management, ongoing mineralization of peat and fluctuating water levels in fen grasslands have overruled effects of current land-use intensity and productivity. Finally, we conclude that regional replication is of major importance for studies seeking general insights into productivity-diversity relationships.

Differenzielles Lehren und Lernen: eine Kritik

Dieser Beitrag beschäftigt sich kritisch mit dem von Wolfgang Schöllhorn seit 1999 propagierten Ansatz des differenziellen Lehrens und Lernens. Nach einer Einordnung in die historische bewegungswissenschaftliche Debatte um den Informationsverarbeitungsansatz und die dynamische Systemtheorie zeigen wir, dass die von Schöllhorn behaupteten Praxiskonsequenzen theoretisch nicht fundiert sind, dass die Abgrenzung zu konkurrierenden Lerntheorien lücken- und fehlerhaft ausfällt, dass die präsentierte empirische Befundlage auf höchst wackeligen Füßen steht und dass der Ansatz sich auch aus Praxissicht als nicht tragfähig erweist. Mit Blick auf fatale Konsequenzen sowohl für die Sportpraxis als auch für die Sportwissenschaft empfehlen wir, in zukünftigen Publikationen zum differenziellen Lernen auf fehlerhafte und theoretisch wie empirisch unbegründete Praxisempfehlungen zu verzichten.

A Donor-Acceptor Tetrathiafulvalene Ligand Complexed to Iron(II): Synthesis, Electrochemistry, and Spectroscopy of Fe(phen)(2)(TTF-dppz)(PF6)(2)

The synthesis and photophysical properties of the complex Fe(phen)(2)(TTF-dppz)(2+) (TTF-dppz = 4',5'-bis-(propylthio)tetrathiafulvenylidipyrido3,2-a:2',3'-c-phenazine, phen = 1,10-phenanthroline) are described. In this complex, excitation into the metal ligand charge transfer bands results in the population of a high-spin state of iron(II), with a decay lifetime of approximately 1.5 ns, in dichloromethane, at room temperature. An intraligand charge transfer state can also be obtained and has a lifetime of 38 ps. A mechanism for the different states reached is proposed based on transient absorption spectroscopy.

Auditive und visuelle Perzeption bei Abseitsentscheidungen im Fussball

Einleitung Die hohe Quote von fehlerhaften Abseitsentscheidungen im Fußball (ca. 26%, Helsen et al., 2006) könnte dadurch erklärt werden, dass Schiedsrichterassistenten zum Zeitpunkt des Passes die Abseitslinie fixieren und den Moment des Passes nur peripher wahr-nehmen (Catteeuw et al., 2009). Diese Annahme wurde geprüft, indem in einem Virtual-Reality-Setting systematisch visuelle (Spielerpositionen) und akustische (Passgeräusch) Informationen manipuliert wurden. Methode In Experiment 1 hatten 28 Teilnehmer die Aufgabe, Abseitsentscheidungen aus der Per-spektive des Schiedsrichterassistenten zu treffen. Dabei wurde das Passgeräusch mani-puliert (Geräusch bei Ballabgabe: 100 ms zu früh, 100 ms zu spät, ohne). Erwartet wurde, dass die Entscheidungsrichtigkeit bei asynchronen Geräuschen sinkt. In Experiment 2 wurde in drei Gruppen die (1) Distanz zum Assistent, (2) Exzentrizität des Passgebers (Winkel zwischen Passgeber und Abseitslinie) oder (3) der zu fixierende Spieler (letzter Verteidiger oder Passgeber) manipuliert. Je Gruppe hatten 20 Teilnehmer die Aufgabe, den Moment des Passes per Knopfdruck anzugeben und Abseitsentscheidungen zu tref-fen. Zu fixierende Orte wurden instruiert und durch Eyetracking geprüft. Prädiziert wurde, dass (1) große Exzentrizitäten und (2) große Entfernungen des Passgebers die Präzision der Passwahrnehmung und die Entscheidungsrichtigkeit senken und (3) der Passmo-ment bei Fixation des Passgebers präziser erkannt wird als bei Fixation des letzten Ver-teidigers. Ergebnisse Die bisher vorliegenden Ergebnisse aus Experiment 1 zeigen, dass die akustische Wahrnehmung des Passes die Entscheidungsrichtigkeit beeinflusst, F(2, 54)= 7.44, p = .01, ηp2 = .22, indem verzögerte Ballgeräusche die Zahl der „Flag-Errors“ (fälschlicher-weise auf Abseits entschieden) erhöht und die der „Non-Flag-Errors“ (Abseits nicht er-kannt) senkt. Experiment 2 wird zeigen, welche Rolle hierbei periphere visuelle Informa-tionen spielen. Diskussion Die vermutete Rückführung von fehlerhaften Abseitsentscheidungen auf periphere (vi-suelle) Wahrnehmungsaspekte konnte bestätigt werden. Der relative Einfluss auditiver und visueller Informationen auf die Fehlerquote gilt es weiter zu untersuchen. Literatur Catteeuw, P., Helsen, W., Gilis, B., Van Roie, E., & Wagemans, J. (2009). Visual scan patterns and decision-making skills of expert assistant referees in offside situations. Journal of Sport & Exercise Psychol-ogy, 31, 786-797. Helsen, W., Gilis, B., & Weston, M. (2006). Errors in judging “offside” in association football: Test of the optical error versus the perceptual flash-lag hypothesis. Journal of Sports Sciences, 24, 521–528.

Palaeoenvironmental changes in Central Europe (NE Poland) during the last 6200 years reconstructed from a high-resolution multi-proxy peat archive

Peat deposits from an ombrotrophic bog (north-eastern Poland) were analysed to reconstruct peatland development and environmental changes. This paper presents reconstructions of hydrological changes and plant succession over the last 6000 years. The methods included the high-resolution analysis of plant macrofossils, pollen and testate amoebae, supported by radiocarbon dating. Three main phases were identified in the history of the bog and surrounding woodland vegetation: 4000–400 BC, 400 BC–AD 1700 and AD 1700–2011. Except for terrestrialisation and the fen-to-bog transition phase, the development of bog vegetation was mainly dependent on the climate until approximately AD 1700. The dominant taxon in Gązwa bog was Sphagnum fuscum/rubellum. Woodland development was significantly affected by human activity at several time periods. The most visible human activity, manifested by the decline of deciduous species, occurred ca. 350 BC, ca. AD 250, ca. AD 1350 and after AD 1700. These events correspond to phases of human settlement in the area. During 400–300 BC, the decline of deciduous trees, primarily Carpinus, coincided with an increase in indicators of human activity and fire frequency. At ca. AD 200, Carpinus and Tilia abundance decreased, corresponding to an increased importance of cereals (Secale and Triticum). Since ca. AD 1350, the impact of Teutonic settlement is apparent, and after AD 1700, deciduous forests largely disappeared.

Magnetic anisotropy in natural amphibole crystals

Anisotropy of magnetic susceptibility (AMS) is often used as a proxy for mineral fabric in deformed rocks. To do so quantitatively, it is necessary to quantify the intrinsic magnetic anisotropy of single crystals of rock-forming minerals. Amphiboles are common in mafic igneous and metamorphic rocks and often define rock texture due to their general prismatic crystal habits. Amphiboles may dominate the magnetic anisotropy in intermediate to felsic igneous rocks and in some metamorphic rock types, because they have a high Fe concentration and they can develop a strong crystallographic preferred orientation. In this study, the AMS is characterized in 28 single crystals and I crystal aggregate of compositionally diverse clino- and ortho-amphiboles. High-field methods were used to isolate the paramagnetic component of the anisotropy, which is unaffected by ferromagnetic inclusions that often occur in amphibole crystals. Laue imaging, laser ablation-inductively coupled plasma-mass spectrometry, and Mossbauer spectroscopy were performed to relate the magnetic anisotropy to crystal structure and Fe concentration. The minimum susceptibility is parallel to the crystallographic a*-axis and the maximum susceptibility is generally parallel to the crystallographic b-axis in tremolite, actinolite, and hornblende. Gedrite has its minimum susceptibility along the a-axis, and maximum susceptibility aligned with c. In richterite, however, the intermediate susceptibility is parallel to the b-axis and the minimum and maximum susceptibility directions are distributed in the a-c plane. The degree of anisotropy, k', increases generally with Fe concentration, following a linear trend: k' = 1.61 x 10(-9) Fe - 1.17 x 10(-9) m(3)/kg. Additionally, it may depend on the Fe2+/Fe3+ ratio. For most samples, the degree of anisotropy increases by a factor of approximately 8 upon cooling from room temperature to 77 K. Fen-oactinolite, one pargasite crystal and riebeckite show a larger increase, which is related to the onset of local ferromagnetic (s.l.) interactions below about 100 K. This comprehensive data set increases our understanding of the magnetic structure of amphiboles, and it is central to interpreting magnetic fabrics of rocks whose AMS is controlled by amphibole minerals.

Present-day vegetation and the Holocene and recent development of Egelsee-Moor, Salzburg province, Austria

This paper describes the present-day vegetation, stratigraphy and developmental history of the mire of Egelsee-Moor (Salzburg, Austria; 45°45′N, 13°8.5′E, 700 m a.s.l., 15 ha in area) since the early Late Glacial on the basis of 4 transects with 14 trial borings across the peatland. We present a vegetation map of the mire, a longitudinal section through the peat body based on six cores showing the peat types, overview macrofossil diagrams of six cores showing the local mire development and two pollen diagrams covering the Late Glacial and Holocene. The chronology of the diagrams depends on biostratigraphic dating for the Late Glacial and early Holocene and radiocarbon dating for the remaining Holocene. The northern part of the mire originated through terrestrialisation of nutrient-rich, mostly inundated fen and the southern part through paludification of wet soils. The very small lake of today was a reservoir until recently for providing water-power for timber rafting (‘Holztrift’). The mire vegetation today is a complex of forested parts (mainly planted Pinus sylvestris and Thuja occidentalis, but also spontaneous Picea abies, Betula pubescens and Frangula alnus), reed-lands (Phragmites) and litter meadows (Molinietum, Schoenetum, etc.). The central part has hummock-hollow complexes with regionally rare species of transitional mires (Drosera anglica, D. intermedia, Lycopodiella inundata, Scorpidium scorpioides, Sphagnum platyphyllum, S. subnitens). The results indicate that some of the mid-Holocene sediments may have been removed by the timber-rafting practices, and that water extraction from the hydrological catchment since 1967 has resulted in a partial shift of transitional mire to ombrotrophic bog. The latter potentially endangers the regionally rare species and was used as an argument to stop further water extraction.