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FIGURE 2 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 2. Habitats at collecting sites. a: Sheko Forest (1570 m); b: Makira Forest (1615 m); c: Dembi Forest (1260 m); d: Bebeka Plantation (1370 m).

FIGURE 3 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 3. Habitats at collecting sites. a: Komba Forest (1860 m); b: Hana Wetland (2425 m); c: Bamboo Forest (2620 m).

FIGURE 37 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 37. Altitudinal variation in males of Neritius abyssinicus. Specimens from higher elevations (left) are significantly larger than those from lower altitudes (right) (Table 4) and are slightly differently coloured. Scale bar represents 1 cm.

FIGURE 32 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 32. Oxya hyla brachypterous form, Shorori wetland (1610 m), Ethiopia. Scale bar represents 1 cm.

FIGURE 4 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 4. Habitats at collecting sites. a: Shorori Wetland (1610 m); b: waterfall at Dembi Forest (1260 m); c: inside the bamboo forest at Bamboo Forest (2620 m).

FIGURE 35 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 35. Eyprepocnemis plorans ibandana, Dembi Forest (1260 m), Ethiopia. Scale bar represents 1 cm.

FIGURE 10 in Orthoptera (Insecta: Tettigonioidea, Pyrgomorphoidea, Acridoidea) of Kafa Biosphere Reserve, Bale Mountains National Park and other areas of conservation interest in Ethiopia

FIGURE 10. Anoedopoda lamellata, Bonga Village (1700 m), Ethiopia (same specimen). Scale bar represents 1 cm.

embargoedcc-by-4.0Jun 2024View details →

Daily European biospheric methane emissions estimated with the ecosystem model JSBACH-HIMMELI.

Daily estimates of European biospheric methane emissions from JSBACH-HIMMELI  model from year 1990 to year 2023. JSBACH-HIMMELI is an ecosystem process model based on JSBACH land surface model, YASSO soil carbon model and HIMMELI methane emission model. The gridded fluxes are available with a resolution of 0.1x0.1 degrees and in units of mol m-2 s-1 (m-2 refers to grid cell area). The gridded flux file contains a variable for methane fluxes, including  a sum of methane fluxes from peatlands, inundated lands and mineral soils. More information of the model set-up is documented in Petrescu, A. M. R., et al., The consolidated European synthesis of CH4 and N2O emissions for the European Union and United Kingdom: 1990–2019, Earth Syst. Sci. Data, 15, 1197–1268, https://doi.org/10.5194/essd-15-1197-2023, 2023, Tyystjärvi, V., 2024. Future methane fluxes of peatlands are controlled by management practices and fluctuations in hydrological conditions due to climatic variability. EGUsphere 1–37. https://doi.org/10.5194/egusphere-2023-3037 and Raivonen, M. et al., 2017. HIMMELI v1.0: HelsinkI Model of MEthane buiLd-up and emIssion for peatlands. Geoscientific Model Development 10, 4665–4691. <a href="https://doi.org/10.5194/gmd-10-4665-2017">https://doi.org/10.5194/gmd-10-4665-2017</a>

opencc-by-4.0Dec 2023View details →

Data from: Constraining biospheric carbon dioxide fluxes by combined top-down and bottom-up approaches

Acknowledgements. We would like to thank Martin Jung, Jakob A. Nelson, Sophia Walther, and the FLUXCOM team for their structural support, feedback and discussion. The Authors would like to thank the producers of the Inversion data included in this study: Ingrid Luijkx and Wouter Peters (CTE), Frederic Chevallier and the Copernicus Atmosphere Monitoring Service (CAMS), Christian Roedenbeck (Jena Carboscope sEXTocNEET), Yosuke Niwa (NISMON-CO2), and Liang Feng and Paul Palmer (UoE). This research was funded by the European Research Council (ERC) Synergy Grant ’Understanding and modeling the Earth System with Machine Learning (USMILE)’ under the Horizon 2020 research and innovation programme (Grant Agreement No. 855187) This work used eddy covariance data acquired by the FLUXNET community and in particular by the following networks: AmeriFlux (U.S. Department of Energy, Biological and Environmental Research, Terrestrial Carbon Program (DE-FG02-04ER63917 and DE-FG02- 04ER63911)), AfriFlux, AsiaFlux, CarboAfrica, CarboEuropeIP, CarboItaly, CarboMont, ChinaFlux, Fluxnet-Canada (supported by CFCAS, NSERC, BIOCAP, Environment Canada, and NRCan), GreenGrass, KoFlux, LBA, NECC, OzFlux, TCOS-Siberia, USCCC. We acknowl- edge the financial support to the eddy covariance data harmonization provided by CarboEuropeIP, FAO-GTOS-TCO, iLEAPS, Max Planck Institute for Biogeochemistry, National Science Foundation, University of Tuscia, Université Laval and Environment Canada and US Depart- ment of Energy and the database development and technical support from Berkeley Water Center, Lawrence Berkeley National Laboratory, Microsoft Research eScience, Oak Ridge National Laboratory, University of California - Berkeley, University of Virginia

opencc-by-4.0Feb 2024View details →

Alignment and Tree file from: Two novel species of tropical Morchella (Ascomycota, Pezizales, Morchellaceae) discovered in the UNESCO Rinjani Lombok Biosphere Reserve, Indonesia

Alignment and Tree file from: Two novel species of tropical Morchella (Ascomycota, Pezizales, Morchellaceae) discovered in the UNESCO Rinjani Lombok Biosphere Reserve, Indonesia

Simulated terrestrial biosphere variables across Termination V (iLOVECLIM model)

The following files contain output data from the 32-kyr iLOVECLIM simulation covering Termination V: both sequences start at 436 kyr BP and end at 404 kyr BP with a yearly time step. <ul> <li>Simulated_carbon_stock.nc: the average simulated carbon stock over latitudinal bands for each of the four carbon components (green biomass, structural biomas, slow Soil Organic Matter (SOM) and fat SOM) and the total carbon stock (sum of the four components).</li> <li>Simulated_tree_fraction.nc: the global simulated tree fraction (in %).</li> </ul>

Fig. 36 in COI mtDNA barcoding and morphology for the description of a new species of ricinuleid of the genus Pseudocellus (Arachnida: Ricinulei: Ricinoididae) from El Triunfo Biosphere Reserve, Chiapas, Mexico

Fig. 36. Species of the genus Pseudocellus Platnick, 1980 described from Chiapas, Mexico, including the new species described herein. Star: El Triunfo Biosphere Reserve, El Quetzal Camp, Angel Albino Corzo Municipality. Red circle: Cerro Boquerón, Ejido Boquerón, Motozintla Municipality. Orange circle: Sumidero del Camino, 16 km NE of Comitán. Pink circle: Kolem-chen Cave "Cueva Grande", Chan-kin Reserve, Ocosingo Municipality. Blue circle: San Francisco Cave, La Trinitaria Municipality. Purple circle: Finca Guatimoc, south slope of the Tacaná volcano, 32 km north of Tapachula, near Cacahuatán. Green circle: Las Abejas Cave, San Fernando Municipality.

Fig. 1 in COI mtDNA barcoding and morphology for the description of a new species of ricinuleid of the genus Pseudocellus (Arachnida: Ricinulei: Ricinoididae) from El Triunfo Biosphere Reserve, Chiapas, Mexico

Fig. 1. Neighbour-Joining (NJ) tree with p-distances constructed with COI barcode sequences from different specimens and species of Pseudocellus Platnick, 1980. Colors of the branches indicate species of Pseudocellus already described, red branches indicate the new species. Numbers on the branches represent Bootstrap support values (>50% significant).

Figs 32–35 in COI mtDNA barcoding and morphology for the description of a new species of ricinuleid of the genus Pseudocellus (Arachnida: Ricinulei: Ricinoididae) from El Triunfo Biosphere Reserve, Chiapas, Mexico

Figs 32–35. Pseudocellus giribeti sp. nov. Paratypes (MCZ 80010). 32–33. Deutonymph, habitus, dorsal and ventral views. 34–35. Tritonymph, habitus, dorsal and ventral views. Scale bars = 2 mm.

Figs 20–26 in COI mtDNA barcoding and morphology for the description of a new species of ricinuleid of the genus Pseudocellus (Arachnida: Ricinulei: Ricinoididae) from El Triunfo Biosphere Reserve, Chiapas, Mexico

Figs 20–26. Pseudocellus giribeti sp. nov. Holotype, ♂ (MCZ 80010). 20–22. Right leg III (copulatory apparatus), retrolateral, prolateral and dorsal views. 23. Copulatory apparatus extended, prolateral view. 24. Copulatory apparatus, dorsal view. 25. Copulatory apparatus, prolateral view. 26. Tarsal process, distal half, prodorsal view. Scale bars: 20–22 = 0.5 mm; 23–25 = 0.2 mm; 26 = 0.1 mm.

Figs 7–10 in COI mtDNA barcoding and morphology for the description of a new species of ricinuleid of the genus Pseudocellus (Arachnida: Ricinulei: Ricinoididae) from El Triunfo Biosphere Reserve, Chiapas, Mexico

Figs 7–10. Pseudocellus giribeti sp. nov. Holotype, ♂ (MCZ 80010). 7–8. Opisthosoma, dorsal and ventral views. 9. Tergite XI, median plate (arrow indicates the lateral depression). 10. Pygidium, posterior view. Scale bars: 7–8 = 1 mm; 9 = 0.5 mm; 10 = 0.2 mm.

Figs 3–6 in COI mtDNA barcoding and morphology for the description of a new species of ricinuleid of the genus Pseudocellus (Arachnida: Ricinulei: Ricinoididae) from El Triunfo Biosphere Reserve, Chiapas, Mexico

Figs 3–6. Pseudocellus giribeti sp. nov. Holotype, ♂ (MCZ 80010). 3–4. Habitus, dorsal and ventral views. 5. Carapace, dorsal view. 6. Prosoma, ventral view, showing coxosternal region. Scale bars: 3–4 = 2 mm; 5–6 = 0.5 mm.

opencc-by-4.0Nov 2021View details →

Are terrestrial biosphere models fit for simulating the global land carbon sink?

This repository contains the data and code required for reproducing the results presented in the paper "Are terrestrial biosphere models fit for simulating the global land carbon sink?" by Seiler et al., 2021. The study evaluates an ensemble of terrestrial biosphere models (<a href="https://sites.exeter.ac.uk/trendy/">TRENDY</a>; v9; S3 simulations) against a wide range of reference data using the Automated Model Benchmarking R package (AMBER; version 1.1.1). The only requirement for reproducing our results is access to a Linux machine with <a href="https://docs.conda.io">conda</a>, an open-source package management system and environment management system, installed. Follow the steps described in the readme file to install AMBER and run the analysis. The repository also contains all output produced by our analysis.

opencc-by-4.0Dec 2021View details →

Figs 9–13 in Scaphisomatini (Coleoptera: Staphylinidae: Scaphidiinae) from two biosphere reserves in eastern China, with descriptions of two new species

Figs 9–13. Habitat of Scaphisoma Leach, 1815 in Wuyishan Mts. 9–10 – Xiaofeng Mountain; 11–13 – Guadun. 9 – general view of broad-leaved forest with bamboo; 10 – detail of sifted microhabitat; 11 – general view of short bamboo forest with intermixed high evergreen trees; 12 – detail of sifted bamboo bush; 13 – border of tea plantation and mixed forest with flowering Castanopsis sp.