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Reports of major losses in insect biodiversity have stimulated an increasing interest in temporal population changes. Existing datasets are often limited to a small number of study sites, few points in time, a narrow range of land‐use intensities and only some taxonomic groups, or they lack standardised sampling. While new monitoring programs have been initiated, they still cover rather short time periods.
Daskalova et al. 2021 (Insect Conservation and Diversity, 14, 1‐18) argue that temporal trends of insect populations derived from short time series are biased towards extreme trends, while their own analysis of an assembly of shorter‐ and longer‐term time series does not support an overall insect decline. With respect to the results of Seibold et al. 2019 (Nature, 574, 671–674) based on a 10‐year multi‐site time series, they claim that the analysis suffers from not accounting for temporal pseudoreplication.
Here, we explain why the criticism of missing statistical rigour in the analysis of Seibold et al. (2019) is not warranted. Models that include ‘year’ as random effect, as suggested by Daskalova et al. (2021), fail to detect non‐linear trends and assume that consecutive years are independent samples which is questionable for insect time‐series data.
We agree with Daskalova et al. (2021) that the assembly and analysis of larger datasets is urgently needed, but it will take time until such datasets are available. Thus, short‐term datasets are highly valuable, should be extended and analysed continually to provide a more detailed understanding of insect population changes under the influence of global change, and to trigger immediate conservation actions.
Recently reported insect declines have raised both political and social concern. Although the declines have been attributed to land use and climate change, supporting evidence suffers from low taxonomic resolution, short time series, a focus on local scales, and the collinearity of the identified drivers. In this study, we conducted a systematic assessment of insect populations in southern Germany, which showed that differences in insect biomass and richness are highly context dependent. We found the largest difference in biomass between semi-natural and urban environments (-42%), whereas differences in total richness (-29%) and the richness of threatened species (-56%) were largest from semi-natural to agricultural environments. These results point to urbanization and agriculture as major drivers of decline. We also found that richness and biomass increase monotonously with increasing temperature, independent of habitat. The contrasting patterns of insect biomass and richness question the use of these indicators as mutual surrogates. Our study provides support for the implementation of more comprehensive measures aimed at habitat restoration in order to halt insect declines.
Episodic low oxygenated conditions on the sea-floor are likely responsible for exceptional preservation of animal remains in the upper Amouslek Formation (lower Cambrian, Stage 3) on the northern slope of the western Anti-Atlas, Morocco. This stratigraphic interval has yielded trilobite, brachiopod, and hyolith fossils with preserved soft parts, including some of the oldest known trilobite guts. The "Souss fossil lagerstatte" (newly proposed designation) represents the first Cambrian fossil lagerstatte in Cambrian strata known from Africa and is one of the oldest trilobite-bearing fossil lagerstatten on Earth. Inter-regional correlation of the Souss fossil lagerstatte in West Gondwana suggests its development during an interval of high eustatic levels recorded by dark shales that occur in informal upper Cambrian Series 2 in Siberia, South China, and East Gondwana.
Bis zum Jahr 2100 prognostiziert der Weltklimarat (IPCC 2021) einen Anstieg des Meeresspiegels von bis zu 63-101 cm gegenüber heutigen Wasserständen. Im Rahmen des Generalplans Küstenschutz Schleswig-Holstein(GKSH) soll als Klimafolgeanpassung eine Erhöhung und Profiländerung der meisten Nordseedeiche und Elbedeiche erfolgen (zusammen 363,3 km mit einer Vegetationsfläche von 3.500 ha). Diese Maßnahmen werden mit einem vollständigen Verlust der alten Deichvegetation einhergehen und zur Freisetzung von großen Mengen an CO₂ aus dem Bodenkohlenstoff führen. Die Seedeiche der Nordseeküste (262 km) zählen zu den artenreichen, semi-natürlichen und von Schafen beweideten Grasländern (Fläche von 2600 ha) in Schleswig-Holstein mit bis zu 18 Gras- und 64 zweikeim-blättrigen Blütenpflanzen und an die Vegetation gebundene 800-1000 Arten von Invertebraten (darunter 200 Käferarten). Auf die Außenböschung dringen Pflanzen der Salzwiesengesellschaften vor. Die steileren, wärmeexponierten (überwiegend nach Osten und Süden ausgerichtet) und durch Vertritt lückigen Innenböschungen der Seedeiche sind wertvolle Refugien wärmeliebender, konkurrenzschwacher Arten von Magerstandorten und Trittgesellschaften wie die folgenden mediterran-subatlantischen Arten: Knotenklettenkerbel (Torilis nodosa), Zwergklee/Armblütiger Klee (Trifolium micranthum) und Vogelfußklee (Trifolium ornithopodioides). Für die Erhaltung beider Kleearten (die aktuelle Verbreitung wird dokumentiert) besitzt Schleswig-Holstein eine nationale und nordwest-europäisch-kontinentale Verantwortlichkeit. Folgende Maßnahmen zum Schutz der reichhaltigen Deichvegetation und Teilen seiner Invertebratenfauna bei der Deichverstärkung im Rahmen des GKSH werden vorgeschlagen: 1. Abheben der Grasnarbe mit Wurzelraum und zeitnahe Wiederverlegung der alten Grasnarbe (Soden) auf das neue Deichprofil; das ist auch wichtig zum Erhalt des Bodenkohlenstoffs (Klimaschutz). 2. Einsaat von neuen Deichprofilen mit Saatgut von artenreichen Deichabschnitten. 3. Aufnahme substanzieller Forschungsprogramme/Forschungsförderung zur Ökologie der Seedeiche. Weiterhin sollte auf den Einsatz von Herbiziden auf Deichen zur Bekämpfung von Disteln verzichtet werden.