Terrestrial invertebrates along a gradient of deglaciation in
Svalbard: Long-term development of soil fauna communities

J 2021

Terrestrial invertebrates along a gradient of deglaciation in Svalbard: Long-term development of soil fauna communities

DEVETTER, Miloslav; Ladislav HANEL; Natalia RASCHMANOVA; Michala BRYNDOVA; Jiří SCHLAGHAMERSKÝ et al.

Základní údaje

Originální název

Terrestrial invertebrates along a gradient of deglaciation in Svalbard: Long-term development of soil fauna communities

Autoři

DEVETTER, Miloslav; Ladislav HANEL; Natalia RASCHMANOVA; Michala BRYNDOVA a Jiří SCHLAGHAMERSKÝ

Vydání

Geoderma, Amsterdam, Elsevier, 2021, 0016-7061

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10618 Ecology

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 7.422

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/21:00120965

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Chronosequences; Glacier Retreat; Deglaciation

Štítky

14314020, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 1. 2021 17:25, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

The recent deglaciation of large polar areas has exposed stretches of land, allowing spontaneous primary succession. The exposed substrate is colonized by soil biota participating in soil formation - a process in which soil characteristics and the biotic community affect each other mutually. Soil fauna was studied along three transects in glacier valleys around Petunia Bay on Svalbard in the High Arctic, representing chronosequences of soil development on plots deglaciated for ten to approximately ten thousand years. Community development was characterised by progressive addition of species, with many pioneer species remaining present throughout soil development. Generally, the abundance and species richness of soil animals increased from the initial to the well-developed sites. Altogether 93 taxa of soil fauna were identified, including 21 species of rotifers, 38 genera of nematodes, 8 species of tardigrades, 21 species of springtails and 4 species of enchytraeids. Rotifers were the earliest colonizers, found already in the initial stage, followed by nematodes in plots several tens of years old. They were followed by tardigrades, which - although in low abundances - established populations in the third stage of the chronosequences, 10(3)-year-old. Collembolans formed stable populations at the end of the chronosequence in the third and fourth stages, 10(3) to 10(4) years old. Enchytraeids only appeared at the end of the chronosequence. Assemblages were significantly driven mostly by the age of the plot, association with a given transect and nutrient availability.

Citovat

DEVETTER, Miloslav; Ladislav HANEL; Natalia RASCHMANOVA; Michala BRYNDOVA a Jiří SCHLAGHAMERSKÝ. Terrestrial invertebrates along a gradient of deglaciation in Svalbard: Long-term development of soil fauna communities. Geoderma. Amsterdam: Elsevier, 2021, roč. 383, February 2021, s. 1-11. ISSN 0016-7061. Dostupné z: https://doi.org/10.1016/j.geoderma.2020.114720.

@article{1727756,
   author = {Devetter, Miloslav and Hanel, Ladislav and Raschmanova, Natalia and Bryndova, Michala and Schlaghamerský, Jiří},
   article_location = {Amsterdam},
   article_number = {February 2021},
   doi = {https://doi.org/10.1016/j.geoderma.2020.114720},
   keywords = {Chronosequences; Glacier Retreat; Deglaciation},
   language = {eng},
   issn = {0016-7061},
   journal = {Geoderma},
   title = {Terrestrial invertebrates along a gradient of deglaciation in Svalbard: Long-term development of soil fauna communities},
   url = {https://doi.org/10.1016/j.geoderma.2020.114720},
   volume = {383},
   year = {2021}
}

TY  - JOUR
ID  - 1727756
AU  - Devetter, Miloslav - Hanel, Ladislav - Raschmanova, Natalia - Bryndova, Michala - Schlaghamerský, Jiří
PY  - 2021
TI  - Terrestrial invertebrates along a gradient of deglaciation in Svalbard: Long-term development of soil fauna communities
JF  - Geoderma
VL  - 383
IS  - February 2021
SP  - 1-11
EP  - 1-11
PB  - Elsevier
SN  - 00167061
KW  - Chronosequences
KW  - Glacier Retreat
KW  - Deglaciation
UR  - https://doi.org/10.1016/j.geoderma.2020.114720
L2  - https://doi.org/10.1016/j.geoderma.2020.114720
N2  - The recent deglaciation of large polar areas has exposed stretches of land, allowing spontaneous primary succession. The exposed substrate is colonized by soil biota participating in soil formation - a process in which soil characteristics and the biotic community affect each other mutually. Soil fauna was studied along three transects in glacier valleys around Petunia Bay on Svalbard in the High Arctic, representing chronosequences of soil development on plots deglaciated for ten to approximately ten thousand years. Community development was characterised by progressive addition of species, with many pioneer species remaining present throughout soil development. Generally, the abundance and species richness of soil animals increased from the initial to the well-developed sites. Altogether 93 taxa of soil fauna were identified, including 21 species of rotifers, 38 genera of nematodes, 8 species of tardigrades, 21 species of springtails and 4 species of enchytraeids. Rotifers were the earliest colonizers, found already in the initial stage, followed by nematodes in plots several tens of years old. They were followed by tardigrades, which - although in low abundances - established populations in the third stage of the chronosequences, 10(3)-year-old. Collembolans formed stable populations at the end of the chronosequence in the third and fourth stages, 10(3) to 10(4) years old. Enchytraeids only appeared at the end of the chronosequence. Assemblages were significantly driven mostly by the age of the plot, association with a given transect and nutrient availability.
ER  -

DEVETTER, Miloslav; Ladislav HANEL; Natalia RASCHMANOVA; Michala BRYNDOVA a Jiří SCHLAGHAMERSKÝ. Terrestrial invertebrates along a gradient of deglaciation in Svalbard: Long-term development of soil fauna communities. \textit{Geoderma}. Amsterdam: Elsevier, 2021, roč.~383, February 2021, s.~1-11. ISSN~0016-7061. Dostupné z: https://doi.org/10.1016/j.geoderma.2020.114720.

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