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Chapin FS, Matson PA and Vitousek P. (2011) *Principles of terrestrial ecosystem ecology: Springer Science and Business Media.*

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Ren Z, Martyniuk N, Oleksy IA, et al. (2019) Ecological stoichiometry of the mountain cryosphere. *Frontiers in Ecology and Evolution* 7: 360.

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Vilmundardóttir OK, Gísladóttir G and Lal R. (2014) Early stage development of selected soil properties along the proglacial moraines of Skaftafellsjökull glacier, SE-Iceland. *Catena* 121: 142-150.

Vreeken Wv. (1975) Principal kinds of chronosequences and their significance in soil history. *Journal of Soil Science* 26: 378-394.

Walker LR. (1999) *Ecosystems of disturbed ground*: Elsevier.

Walker LR and del Moral R. (2003) *Primary succession and ecosystem rehabilitation*: Cambridge University Press.

Walker LR and del Moral R. (2009) Lessons from primary succession for restoration of severely damaged habitats. *Applied Vegetation Science* 12: 55-67.

Walker LR and del Moral R. (2011) Primary Succession. eLS. John Wiley and Sons, Ltd: Chichester.

Walker LR and Wardle DA. (2014) Plant succession as an integrator of contrasting ecological time scales. *Trends in ecology and evolution* 29: 504-510.

Walker LR, Wardle DA, Bardgett RD, et al. (2010) The use of chronosequences in studies of ecological succession and soil development. *Journal of Ecology* 98: 725-736.
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Vellend M. (2010) Conceptual synthesis in community ecology. *The Quarterly review of biology* 85: 183-206.

Vilmundardóttir O, Gísladóttir G and Lal R. (2015) Between ice and ocean; soil development along an age chronosequence formed by the retreating Breiðamerkurjökull glacier, SE-Iceland. *Geoderma* 259: 310-320.

Vilmundardóttir OK, Gísladóttir G and Lal R. (2014) Early stage development of selected soil properties along the proglacial moraines of Skaftafellsjökull glacier, SE-Iceland. *Catena* 121: 142-150.

Vreeken Wv. (1975) Principal kinds of chronosequences and their significance in soil history. *Journal of Soil Science* 26: 378-394.

Walker LR. (1999) *Ecosystems of disturbed ground*: Elsevier.

Walker LR and del Moral R. (2003) *Primary succession and ecosystem rehabilitation*: Cambridge University Press.

Walker LR and del Moral R. (2009) Lessons from primary succession for restoration of severely damaged habitats. *Applied Vegetation Science* 12: 55-67.

Walker LR and del Moral R. (2011) Primary Succession. eLS. John Wiley and Sons, Ltd: Chichester.

Walker LR and Wardle DA. (2014) Plant succession as an integrator of contrasting ecological time scales. *Trends in ecology and evolution* 29: 504-510.

Walker LR, Wardle DA, Bardgett RD, et al. (2010) The use of chronosequences in studies of ecological succession and soil development. *Journal of Ecology* 98: 725-736.
Walker LR and Willig MR. (1999) An introduction to terrestrial disturbances. *Ecosystems of the World*: 1-16.

Ward JV, Malard F, Tockner K, et al. (1999) Influence of ground water on surface water conditions in a glacial flood plain of the Swiss Alps. *Hydrological Processes* 13: 277-293.

Wardle P. (1980) Primary succession in Westland national park and its vicinity, New Zealand. *New Zealand journal of botany* 18: 221-232.

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Willig MR and Walker LR. (1999) Disturbance in terrestrial ecosystems: salient themes, synthesis, and future directions. *Ecosystems of the World*: 747-768.

Witherow RA, Lyons WB, Bertler NA, et al. (2006) The aeolian flux of calcium, chloride and nitrate to the McMurdo Dry Valleys landscape: evidence from snow pit analysis. *Antarctic Science* 18: 497-505.

Wojcik R, Donhauser J, Frey B, and Benning L.G. (2020). Time since deglaciation and geomorphological disturbances determine the patterns of geochemical, mineralogical and microbial successions in an Icelandic foreland. *Geoderma* 379: 1145-1178.

Wojcik R, Donhauser J, Frey B, et al. (2018) Linkages between geochemistry and microbiology in a proglacial terrain in the High Arctic. *Annals of Glaciology* 59: 95-110.

Wojcik R, Palmtag J, Hugelius G, et al. (2019) Land cover and landform-based upscaling of soil organic carbon stocks on the Brøgger Peninsula, Svalbard. *Arctic, Antarctic, and Alpine Research* 51: 40-57.

Wynn P and Hodson A. (2007) Nitrate production beneath a High Arctic glacier, Svalbard. Chem.
Walker LR and Willig MR. (1999) An introduction to terrestrial disturbances. *Ecosystems of the World*: 1-16.

Ward JV, Malard F, Tockner K, et al. (1999) Influence of ground water on surface water conditions in a glacial flood plain of the Swiss Alps. *Hydrological Processes* 13: 277-293.

Wardle P. (1980) Primary succession in Westland national park and its vicinity, New Zealand. *New Zealand journal of botany* 18: 221-232.

Welch D. (1970) Substitution of space for time in a study of slope development. *The Journal of Geology* 78: 234-239.

Whittaker RJ. (1989) The vegetation of the Storbreen gletschervorfeld, Jotunheimen, Norway. III. Vegetation-environment relationships. *Journal of Biogeography*: 413-433.

Whittaker RJ. (1991) The vegetation of the Storbreen gletschervorfeld, Jotunheimen, Norway. IV. Short-term vegetation change. *Journal of Biogeography*: 41-52.

Wietrzyk P, Węgrzyn M and Lisowska M. (2016) Vegetation diversity and selected abiotic factors influencing the primary succession process on the forefield of Gåsbreen, Svalbard. *Polish Polar Research*: 493-509.

Willemse NW, Koster EA, Hoogakker B, et al. (2003) A continuous record of Holocene eolian activity in West Greenland. *Quaternary Research* 59: 322-334.

Willig MR and Walker LR. (1999) Disturbance in terrestrial ecosystems: salient themes, synthesis, and future directions. *Ecosystems of the World*: 747-768.

Witherow RA, Lyons WB, Bertler NA, et al. (2006) The aeolian flux of calcium, chloride and nitrate to the McMurdo Dry Valleys landscape: evidence from snow pit analysis. *Antarctic Science* 18: 497-505.

Wojcik R, Donhauser J, Frey B and Benning L.G. (2020). Time since deglaciation and geomorphological disturbances determine the patterns of geochemical, mineralogical and microbial successions in an Icelandic foreland. *Geoderma* 379: 1145-1178.

Wojcik R, Donhauser J, Frey B, et al. (2018) Linkages between geochemistry and microbiology in a proglacial terrain in the High Arctic. *Annals of Glaciology* 59: 95-110.

Wojcik R, Palmtag J, Hugelius G, et al. (2019) Land cover and landform-based upscaling of soil organic carbon stocks on the Brøgger Peninsula, Svalbard. *Arctic, Antarctic, and Alpine Research* 51: 40-57.

Wynn P and Hodson A. (2007) Nitrate production beneath a High Arctic glacier, Svalbard. Chem.
Geol. 244: 88-102.

Xiaodong L, Liguang S and Xuebin Y. (2004) Textural and geochemical characteristics of proglacial sediments: A case study in the forefield of the Nelson Ice Cap, Antarctica. *Acta Geologica Sinica-English Edition* 78: 970-981.

Yariv S and Cross H. (2001) *Organo-clay complexes and interactions*: CRC Press.

Yoo K, Amundson R, Heimsath AM, et al. (2006) Spatial patterns of soil organic carbon on hillslopes: Integrating geomorphic processes and the biological C cycle. *Geoderma* 103: 47-65.

Yoo K, Amundson R, Heimsath AM, et al. (2007) Integration of geochemical mass balance with sediment transport to calculate rates of soil chemical weathering and transport on hillslopes. *Journal of Geophysical Research: Earth Surface* 112.

Zdanowski MK, Żmuda-Baranowska MJ, Borsuk P, et al. (2013) Culturable bacteria community development in postglacial soils of Ecology Glacier, King George Island, Antarctica. *Polar Biology* 36: 511-527.

Zender CS, Newman D and Torres O. (2003) Spatial heterogeneity in aeolian erodibility: Uniform, topographic, geomorphic, and hydrologic hypotheses. *Journal of Geophysical Research: Atmospheres* 108.

Zinger L, Shahnavaz B, Baptist F, et al. (2009) Microbial diversity in alpine tundra soils correlates with snow cover dynamics. *The ISME journal* 3: 850-859.

Zumsteg A, Bååth E, Stierli B, et al. (2013) Bacterial and fungal community responses to reciprocal soil transfer along a temperature and soil moisture gradient in a glacier forefield. *Soil Biology and Biochemistry* 61: 121-132.

Zumsteg A, Luster J, Göransson H, et al. (2012) Bacterial, archaeal and fungal succession in the forefield of a receding glacier. *Microbial ecology* 63: 552-564.

Zwoliński Z, Giżejewski J, Karczewski A, et al. (2013) Geomorphological settings of Polish research areas on Spitsbergen. *Landform Analysis* 22.
Geol. 244: 88-102.

Xiaodong L, Liguang S and Xuebin Y. (2004) Textural and geochemical characteristics of proglacial sediments: A case study in the forefield of the Nelson Ice Cap, Antarctica. *Acta Geologica Sinica-English Edition* 78: 970-981.

Yariv S and Cross H. (2001) *Organo-clay complexes and interactions*: CRC Press.

Yoo K, Amundson R, Heimsath AM, et al. (2006) Spatial patterns of soil organic carbon on hillslopes: Integrating geomorphic processes and the biological C cycle. *Geoderma* 103: 47-65.

Yoo K, Amundson R, Heimsath AM, et al. (2007) Integration of geochemical mass balance with sediment transport to calculate rates of soil chemical weathering and transport on hillslopes. *Journal of Geophysical Research: Earth Surface* 112.

Zdanowski MK, Żmuda-Baranowska MJ, Borsuk P, et al. (2013) Culturable bacteria community development in postglacial soils of Ecology Glacier, King George Island, Antarctica. *Polar Biology* 36: 511-527.

Zender CS, Newman D and Torres O. (2003) Spatial heterogeneity in aeolian erodibility: Uniform, topographic, geomorphic, and hydrologic hypotheses. *Journal of Geophysical Research: Atmospheres* 108.

Zinger L, Shahnavaz B, Baptist F, et al. (2009) Microbial diversity in alpine tundra soils correlates with snow cover dynamics. *The ISME journal* 3: 850-859.

Zumsteg A, Bååth E, Stierli B, et al. (2013) Bacterial and fungal community responses to reciprocal soil transfer along a temperature and soil moisture gradient in a glacier forefield. *Soil Biology and Biochemistry* 61: 121-132.

Zumsteg A, Luster J, Göransson H, et al. (2012) Bacterial, archaeal and fungal succession in the forefield of a receding glacier. *Microbial ecology* 63: 552-564.

Zwoliński Z, Giżejewski J, Karczewski A, et al. (2013) Geomorphological settings of Polish research areas on Spitsbergen. *Landform Analysis* 22.