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Platform data

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Please refer to "Ließ et al. (2016), Improving the spatial prediction of soil organic carbon stocks in a complex tropical mountain landscape by methodological specifications in machine learning approaches. PLoS ONE, 11(4): e0153673. doi:10.1371/journal.pone.0153673" for further datails.

The mycobionts of 103 terrestrial and epiphytic orchid individuals, sampled in the RBSF from permanently estabished orchid plots, were identified by sequencing the whole ITS1-5.8S-ITS2 region and part of 28S rDNA. Tulasnellales, Sebacinales and for the first time Atractiellales were found.

Plots were established by members of UTPL, Dr. Juan Pablo Suarez and his coworkers, on the orchid regeneration land slide, on basis of T1 and in uppar part of T2 as given by geographic parameters. All laboratory work was carried out by the UTPL group mentioned above.

Position of trees in the natural forest experiment was calculated using trigonometric measurements from 2004 and 2009. Precision is estimated to be between 0-10m.

Orthomosaic containing Georeferenced NDVI Values from ecsf forest aquired with a low flying UAV.

Monthly measurement of soil temperature and soil gas fluxes (CO2, N2O) in the NUMEX plots in Bombuscaro, ECSF und Cajanuma

Monthly measurements of gas fluxes were performed using static vented chambers.
Soil temperature was taken simultaneously with gas measurements.

Soil texture were sampled in the young landslide in front of the station, on the other side of the San Francisco river. Soil samples were analysed in the laboratory of the University of Bayreuth.

Orthomosaic containing Georeferenced RGB Imagery from ECSF forest aquired with a low flying UAV.

Corrected plots from Bombuscaro, ECSF, Cajanuma, Zamora and Laipuna region as shape files.

Weekly time series of throughfall data from the ECSF area in the microcatchment Q2 (transects Q2.1, Q2.2 and Q2.3). Throughfall was measured weekly with 20 Hellmann-type pluviometers at each transect. The weekly replicates were volume-weighted and bulked to one sample per collecting interval and transect. Electrical conductivity and pH values were measured immediately in unfiltered aliquots in the laboratory at the ECSF.

näheres siehe Artikel: Bräuning, A., Volland-Voigt, F., Burchardt, I., Ganzhi, O., Nauss, T. & Peters, T.: Climatic control of radial growth of Cedrela montana in a humid mountain rain forest in southern Ecuador. In: Erdkunde 59 (4)

"Orthomosaic containing Georeferenced Band Values from Laipuna pasture acquired with a low flying UAV."

Abundance of vascular epiphytes (incl. hemiepiphytes) in 10 x 10 m plots across a land-use gradient.
All samples (columns) give abundance data for vascular epiphyte assemblages in plots of 10x10 meters. PT = Handtuchfläche secondary forest (RSF), Ai = secondary forest at Arco Iris (Ai1: around Ai-building, Ai2-plots on neighbouring ridge towards W), Q2 = Quebrada 2 (RSF), Q5 = Quebrada 5 (RSF), PP = Pinus plantation above ECSF, LC = Loma Chamusqiuín (1-4: secondary forest below Loja-Zamora road, 5-8: secondary forest above Loja-Zamora road). SF = tall secondary forest at RSF, DF = tall degraded forest at RSF; MF = mature (undisturbed) forest at RSF.
Geogr. coordenates still need to be added.
Contact: florianwerner@yahoo.com

Beschreibung: Hier sind die Ergebnisse der Auswertungen der hemisphärischen Bilder mit dem Programm HemiView Canopy Analysis Software (Version 2.1 SR1, Delta T Devices Ltd., www.delta-t.co.uk) angegeben.
Weiterhin sind die Ergebnisse der Vermessungen an den Messpunkten angegeben.
In der Übersicht sind die Mittelwerte (Zeile 6-14), die Standardabweichungen (Zeile 23-31) und die Variationskoeffizienten (Zeile 40-48) angegeben.
Qualität: Mittelwerte aus den Rohdaten (9 Einzelmessstellen im Plot)
Angegebene Literatur: Anderson, M.C. 1964a. Light relations of terrestrial plant communities and their measurement. Biological Reviews 39:425-486. 
Anderson, M.C. 1964b. Studies of the woodland light climate I. The photographic computation of light condition. Journal of Ecology 52:27-41. 
Anderson, M.C. 1964c. Studies of the woodland light climate. II. seasonal variation in the light climate. Journal of Ecology 52:643-663. 
Campbell, G.S. 1986 Extinction coefficients for radiation in plant canopies calculated using an ellipsoidal inclination angle distribution. Agricultural & Forest Meteorology, 36:317 - 321.

Original data: FOR402 (Phase 2) ID: 50655-50663; Creators: Dalitz, Helmut and Oesker, Mathias (AG:  B2-B2)
 
This dataset has been migrated from the previous FOR402-Database to the FOR816-Database by the Central Data Management Z1/FOR816.
Please keep in mind that the migration included all avilable metainfomation which were accessible through the FOR402-Database. Nevertheless, it can't be guaranteed that no thematic misinterpretation occured in the data/attribute description.
There has been no further disciplin specfic control. In any case of ambiguity please contact the dataset creator.

The table is a  list of arbuscular mycorrhizal fungi with their host plants. The sequences are deposited in the NCBI GenBank.

Weekly time series of precipitation data from the San Francisco area at 2000 m a.s.l. at the measuring station FN2 located at the intersection of Camino Canal and Camino Zig-Zag. Precipitation was measured with 5 Hellmann-type pluviometers. The resulting weekly replicates of precipitation were volume-weighted and bulked to one sample per collecting interval. Electrical conductivity and pH values were measured immediately in unfiltered aliquots in the laboratory at the ECSF.

Aggregated values from 1998 are incomplete (March to December).

Quality assessment ECSF climate station hourly data: Version 2; Dataset supersedes ver. 1 which is left for reference. Please be aware, that aggregated values may be wrong, due to the data gaps. This is especcially critical for precipitation. Variables: Ta2m =Air Temperature at 2 m (T) PCP = Precipitation at 1 m (P) Huma_2m = relative humidity at 2m (rH) Irradiation = global radiation at 2 m (gRad), widspeed. Emitted radiation, wind direction and soil-temperatures are not yet published For each variable, a measure of uncertainty is given in the original dimension. This value can be considered as the potential deviation from real conditions. Where no parallel measurements exist, the uncertainty is given as the standard deviation of that difference. By Rütger Rollenbeck, 25.11.2015, rollenbeck@lcrs.de

Details of data processing are given in the attached Qualityassessment-Document

Orthomosaic containing Georeferenced Band Values from ecsf pasture aquired with a low flying UAV.