Descripción
This study aims to do a repeated survey along two proglacial chronosequences near Kongsfjorden, Svalbard. This study will revisit and sample the same sites as those studied by Hodkinson et al. (2004) in their work "invertebrate community assembly along proglacial chronosequences in the high Arctic". their study demonstrated that the succession was predictable, directional and deterministic closely linked to plant colonisation, soil development and species specific traits.
Since the study was conducted in 2004 climate change has increased temperatures causing the glacier to further retreat. With temperatures in Svalbard increasing with approximately four degrees in the past century. The Arctic is particularly vulnerable to climate change due to a phenomenon known as Arctic amplification, whereby the region is warming up to four times faster than the global average.
In addition to analysing community assembly and assessing explanatory abiotic/biotic factors, we're also evaluating potential climate-driven shift in colonisation patterns.
Registros
Los datos en este recurso de registros biológicos han sido publicados como Archivo Darwin Core(DwC-A), el cual es un formato estándar para compartir datos de biodiversidad como un conjunto de una o más tablas de datos. La tabla de datos del core contiene 228 registros.
Este IPT archiva los datos y, por lo tanto, sirve como repositorio de datos. Los datos y los metadatos del recurso están disponibles para su descarga en la sección descargas. La tabla versiones enumera otras versiones del recurso que se han puesto a disposición del público y permite seguir los cambios realizados en el recurso a lo largo del tiempo.
Versiones
La siguiente tabla muestra sólo las versiones publicadas del recurso que son de acceso público.
Derechos
Los usuarios deben respetar los siguientes derechos de uso:
El publicador y propietario de los derechos de este trabajo es The University Centre in Svalbard. Esta obra está bajo una licencia Creative Commons de Atribución/Reconocimiento (CC-BY 4.0).
Registro GBIF
Este recurso ha sido registrado en GBIF con el siguiente UUID: a93a9b5b-1240-4163-8eb4-b4775620d91e. The University Centre in Svalbard publica este recurso y está registrado en GBIF como un publicador de datos avalado por GBIF Norway.
Palabras clave
Earth Science > Biosphere > Ecosystems > Terrestrial ecosystems > Alpine/Tundra > Arctic tundra; Earth science > Biological classification > Animals/invertebrates; Earth science > Human dimensions > Climate change responses; Earth science > Biosphere > Ecological dynamics > Community dynamics > Plant succession; Earth science > Agriculture > Soils > Soil pH; Earth science > Agriculture > Soils > Soil moisture/water content; Earth science > Agriculture > Soils > Carbon; Occurrence; Observation
Contactos
- Originador
Cobertura geográfica
Kongsfjorden NYA - Lovénbreen, Storholmen, Midtholmen.
| Coordenadas límite | Latitud Mínima Longitud Mínima [78,892, 12,072], Latitud Máxima Longitud Máxima [78,935, 12,299] |
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Cobertura taxonómica
No hay descripción disponible
| Reino | Animalia |
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| Filo | Arthropoda |
| Class | Enthognatha, Insecta, Arachnida |
| Orden | Acari, Araneae, Collembola |
Datos del proyecto
No hay descripción disponible
| Título | UNIS AB-201 |
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| Identificador | https://www.wikidata.org/wiki/Q119442230 |
Personas asociadas al proyecto:
- Investigador Principal
Métodos de muestreo
At each site three plots were established, selected based on the presence of either Saxifraga oppositifolia or Salix polaris and each plot had to be at least 10 meters apart. From each plot, two invertebrate samples were extracted containing one of the two focal plant species. Moisture content of the local sample area was measured and noted with a Delta-T SM150 moisture-meter. Afterwards, the samples were cut 10x10x10 centimeters with a knife, using a piece of cardboard as template and extracted with the help of a trowel where the organic layer depth was measured with a ruler (average of 4 sides of the square) as well as determining the observed parental soil type as described in the field protocol, appendix XX. Furthermore, UTM coordinates and date and time were noted for each sample. The samples were stored in, partially closed (sufficient breathing room for the invertebrate species), zip-lock bags in a 5 degrees Celsius fridge to be used for Tullgren-funnel-extraction of invertebrates. In addition to the six invertebrate samples, 3 soil samples were also sampled from each site. The soil sample’s requirements were to be extracted next to Saxifraga oppositifolia and Salix polaris with the third soil sample being extracted from a “random” spot within the site. The soil samples were handled with latex gloves to prevent human contamination, as skin flakes and sweat contain organic carbon and nitrogen, which could alter the sample's C/N ratio and make the analysis unreliable. Furthermore, UTM coordinates and date and time were noted for each sample. The soil samples were stored in labeled zip-lock bags, unrefrigerated and airtight, to be used for pH measurement, C/N analysis and organic matter content.
| Área de Estudio | In total, our study included ten different sampling sites (Fig. 1). Site one through seven were the same sites used by Hodkinson et al. (2003), as shown in figure 1. The sampling sites form a chronosequence in the proglacial area of a land-terminating glacier, the Midtre Lovénbre SE of Ny-Ålesund, and represent a gradient of time exposed to the atmosphere, post-glacial retreat, where new land can be colonized by the surrounding flora and fauna. Site one to seven were located in-field via the coordinates cited in Hodkinson et al. (2003), using a Garmin eTrex GPS. Site zero, not featured in existing studies, was chosen based on recent satellite images and confirmed in the field as a suitable and relatively flat area. The age of this site was determined using Landsat 8-9 satellite imagery, identifying the absence of snow during summer months from 2023 onwards (EROS, 2013). The two additional sample sites, Midtholmen and Storholmen, located NE of Ny-Ålesund, are small islands in Kongsfjord that were released successively from beneath the ice during the regression of the main valley glacier, the Kongsbre. These islands lie 3 km from the mainland shore and are separated by approximately 1 km of open water. Unlike the mainland sites, the Lovén Island communities developed on glacial diamicton, receiving a substantial influx of nutrients from surrounding marine ecosystems (Alsos, Elvebakk & Gabrielsen 1998; Hodkinson et al. 2003). While the general sampling protocol for the islands was identical to that used at the glacier sites, the three plots for each island were intentionally spread out to ensure coverage of the whole island. |
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Descripción de la metodología paso a paso:
- N/A
Metadatos adicionales
| Agradecimientos | Thank you to Anna Seniczak for her expertise and guidance in invertebrate identification. |
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| Identificadores alternativos | https://ipt.gbif.no/resource?r=chronosequence_invertebrates |