How the most northern lizard, Zootoca vivipara, overwinters in Siberia

Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our res...
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Autor*in:	Berman, Daniil I. [verfasserIn] Bulakhova, Nina A. Alfimov, Arcady V. Meshcheryakova, Ekaterina N.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2016

Schlagwörter:	Cold hardiness Hibernacula Range Yakutia Talik zones

Anmerkung:	© Springer-Verlag Berlin Heidelberg 2016

Übergeordnetes Werk:	Enthalten in: Polar biology - Berlin : Springer, 1982, 39(2016), 12 vom: 11. März, Seite 2411-2425
Übergeordnetes Werk:	volume:39 ; year:2016 ; number:12 ; day:11 ; month:03 ; pages:2411-2425

Links:	Volltext

DOI / URN:	10.1007/s00300-016-1916-z

Katalog-ID:	SPR003941183

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520			\|a Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit.
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700	1		\|a Alfimov, Arcady V. \|4 aut
700	1		\|a Meshcheryakova, Ekaterina N. \|4 aut
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912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_101
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_267
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_381
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
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912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_2548
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4046
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
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912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
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912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
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952			\|d 39 \|j 2016 \|e 12 \|b 11 \|c 03 \|h 2411-2425

Indexfelder

author_variant	d i b di dib n a b na nab a v a av ava e n m en enm
matchkey_str	article:14322056:2016----::oteototeniadotcvvproe
hierarchy_sort_str	2016
publishDate	2016
allfields	10.1007/s00300-016-1916-z doi (DE-627)SPR003941183 (SPR)s00300-016-1916-z-e DE-627 ger DE-627 rakwb eng Berman, Daniil I. verfasserin aut How the most northern lizard, Zootoca vivipara, overwinters in Siberia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. Cold hardiness (dpeaa)DE-He213 Hibernacula (dpeaa)DE-He213 Range (dpeaa)DE-He213 Yakutia (dpeaa)DE-He213 Talik zones (dpeaa)DE-He213 Bulakhova, Nina A. (orcid)0000-0002-3000-6476 aut Alfimov, Arcady V. aut Meshcheryakova, Ekaterina N. aut Enthalten in Polar biology Berlin : Springer, 1982 39(2016), 12 vom: 11. März, Seite 2411-2425 (DE-627)271175427 (DE-600)1478942-5 1432-2056 nnns volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425 https://dx.doi.org/10.1007/s00300-016-1916-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2016 12 11 03 2411-2425
spelling	10.1007/s00300-016-1916-z doi (DE-627)SPR003941183 (SPR)s00300-016-1916-z-e DE-627 ger DE-627 rakwb eng Berman, Daniil I. verfasserin aut How the most northern lizard, Zootoca vivipara, overwinters in Siberia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. Cold hardiness (dpeaa)DE-He213 Hibernacula (dpeaa)DE-He213 Range (dpeaa)DE-He213 Yakutia (dpeaa)DE-He213 Talik zones (dpeaa)DE-He213 Bulakhova, Nina A. (orcid)0000-0002-3000-6476 aut Alfimov, Arcady V. aut Meshcheryakova, Ekaterina N. aut Enthalten in Polar biology Berlin : Springer, 1982 39(2016), 12 vom: 11. März, Seite 2411-2425 (DE-627)271175427 (DE-600)1478942-5 1432-2056 nnns volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425 https://dx.doi.org/10.1007/s00300-016-1916-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2016 12 11 03 2411-2425
allfields_unstemmed	10.1007/s00300-016-1916-z doi (DE-627)SPR003941183 (SPR)s00300-016-1916-z-e DE-627 ger DE-627 rakwb eng Berman, Daniil I. verfasserin aut How the most northern lizard, Zootoca vivipara, overwinters in Siberia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. Cold hardiness (dpeaa)DE-He213 Hibernacula (dpeaa)DE-He213 Range (dpeaa)DE-He213 Yakutia (dpeaa)DE-He213 Talik zones (dpeaa)DE-He213 Bulakhova, Nina A. (orcid)0000-0002-3000-6476 aut Alfimov, Arcady V. aut Meshcheryakova, Ekaterina N. aut Enthalten in Polar biology Berlin : Springer, 1982 39(2016), 12 vom: 11. März, Seite 2411-2425 (DE-627)271175427 (DE-600)1478942-5 1432-2056 nnns volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425 https://dx.doi.org/10.1007/s00300-016-1916-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2016 12 11 03 2411-2425
allfieldsGer	10.1007/s00300-016-1916-z doi (DE-627)SPR003941183 (SPR)s00300-016-1916-z-e DE-627 ger DE-627 rakwb eng Berman, Daniil I. verfasserin aut How the most northern lizard, Zootoca vivipara, overwinters in Siberia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. Cold hardiness (dpeaa)DE-He213 Hibernacula (dpeaa)DE-He213 Range (dpeaa)DE-He213 Yakutia (dpeaa)DE-He213 Talik zones (dpeaa)DE-He213 Bulakhova, Nina A. (orcid)0000-0002-3000-6476 aut Alfimov, Arcady V. aut Meshcheryakova, Ekaterina N. aut Enthalten in Polar biology Berlin : Springer, 1982 39(2016), 12 vom: 11. März, Seite 2411-2425 (DE-627)271175427 (DE-600)1478942-5 1432-2056 nnns volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425 https://dx.doi.org/10.1007/s00300-016-1916-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2016 12 11 03 2411-2425
allfieldsSound	10.1007/s00300-016-1916-z doi (DE-627)SPR003941183 (SPR)s00300-016-1916-z-e DE-627 ger DE-627 rakwb eng Berman, Daniil I. verfasserin aut How the most northern lizard, Zootoca vivipara, overwinters in Siberia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. Cold hardiness (dpeaa)DE-He213 Hibernacula (dpeaa)DE-He213 Range (dpeaa)DE-He213 Yakutia (dpeaa)DE-He213 Talik zones (dpeaa)DE-He213 Bulakhova, Nina A. (orcid)0000-0002-3000-6476 aut Alfimov, Arcady V. aut Meshcheryakova, Ekaterina N. aut Enthalten in Polar biology Berlin : Springer, 1982 39(2016), 12 vom: 11. März, Seite 2411-2425 (DE-627)271175427 (DE-600)1478942-5 1432-2056 nnns volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425 https://dx.doi.org/10.1007/s00300-016-1916-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2016 12 11 03 2411-2425
language	English
source	Enthalten in Polar biology 39(2016), 12 vom: 11. März, Seite 2411-2425 volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425
sourceStr	Enthalten in Polar biology 39(2016), 12 vom: 11. März, Seite 2411-2425 volume:39 year:2016 number:12 day:11 month:03 pages:2411-2425
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Cold hardiness Hibernacula Range Yakutia Talik zones
isfreeaccess_bool	false
container_title	Polar biology
authorswithroles_txt_mv	Berman, Daniil I. @@aut@@ Bulakhova, Nina A. @@aut@@ Alfimov, Arcady V. @@aut@@ Meshcheryakova, Ekaterina N. @@aut@@
publishDateDaySort_date	2016-03-11T00:00:00Z
hierarchy_top_id	271175427
id	SPR003941183
language_de	englisch
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author	Berman, Daniil I.
spellingShingle	Berman, Daniil I. misc Cold hardiness misc Hibernacula misc Range misc Yakutia misc Talik zones How the most northern lizard, Zootoca vivipara, overwinters in Siberia
authorStr	Berman, Daniil I.
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topic_title	How the most northern lizard, Zootoca vivipara, overwinters in Siberia Cold hardiness (dpeaa)DE-He213 Hibernacula (dpeaa)DE-He213 Range (dpeaa)DE-He213 Yakutia (dpeaa)DE-He213 Talik zones (dpeaa)DE-He213
topic	misc Cold hardiness misc Hibernacula misc Range misc Yakutia misc Talik zones
topic_unstemmed	misc Cold hardiness misc Hibernacula misc Range misc Yakutia misc Talik zones
topic_browse	misc Cold hardiness misc Hibernacula misc Range misc Yakutia misc Talik zones
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title	How the most northern lizard, Zootoca vivipara, overwinters in Siberia
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title_full	How the most northern lizard, Zootoca vivipara, overwinters in Siberia
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author_browse	Berman, Daniil I. Bulakhova, Nina A. Alfimov, Arcady V. Meshcheryakova, Ekaterina N.
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title_sort	how the most northern lizard, zootoca vivipara, overwinters in siberia
title_auth	How the most northern lizard, Zootoca vivipara, overwinters in Siberia
abstract	Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. © Springer-Verlag Berlin Heidelberg 2016
abstractGer	Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. © Springer-Verlag Berlin Heidelberg 2016
abstract_unstemmed	Abstract The common lizard Zootoca vivipara has the largest range of all the terrestrial reptiles which includes the subarctic regions of the Palaearctic. The species provides a unique model for studying the strategies of adaptation of a reptile to extreme low winter temperatures. The aim of our research was to determine whether this species survives the severe winters of Siberia, including Yakutia, due to its exceptional cold hardiness or due to wintering in abnormally warm places. The cold hardiness limit of lizards from the southeast of Western Siberia was lower than in conspecific European populations (−4 °C) and was the record low for all adult reptiles. In dry substrate (water content 13–14 %), 21 % of lizards survived at temperatures from −3 to −10 °C, but in wet substrate (70–80 %) none of them survived even at slightly below-zero temperatures. The survivors remained in a supercooled state until the temperature dropped to about −3 °C, and then they froze and could remain frozen for over 2 months. In most biotopes examined in the southeast of Western Siberia, soil temperatures at the depth of the lizard hibernacula (5–13 cm) were higher than −10 °C. Despite very cold air, similar winter soil temperatures were recorded in the warmest lizard habitats in Yakutia, due to the soil-heating effect of unfrozen groundwater in talik zones. Thus, extensive distribution of the common lizard in Yakutia is determined not only by its exceptional cold hardiness but also by specific hydrogeological conditions maintaining winter soil temperatures above its tolerance limit. © Springer-Verlag Berlin Heidelberg 2016
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container_issue	12
title_short	How the most northern lizard, Zootoca vivipara, overwinters in Siberia
url	https://dx.doi.org/10.1007/s00300-016-1916-z
remote_bool	true
author2	Bulakhova, Nina A. Alfimov, Arcady V. Meshcheryakova, Ekaterina N.
author2Str	Bulakhova, Nina A. Alfimov, Arcady V. Meshcheryakova, Ekaterina N.
ppnlink	271175427
mediatype_str_mv	c
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1007/s00300-016-1916-z
up_date	2024-07-03T22:39:48.929Z
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How the most northern lizard, Zootoca vivipara, overwinters in Siberia

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