A first chironomid-based summer temperature reconstruction
(13-5 ka BP) around 49 degrees N in inland Europe compared with
local lake development

J 2016

A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development

HÁJKOVÁ, Petra, Petr PAŘIL, Libor PETR, Barbora CHATTOVÁ, Tomáš Matys GRYGAR et. al.

Základní údaje

Originální název

A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development

Autoři

HÁJKOVÁ, Petra (203 Česká republika, garant, domácí), Petr PAŘIL (203 Česká republika, domácí), Libor PETR (203 Česká republika, domácí), Barbora CHATTOVÁ (203 Česká republika, domácí), Tomáš Matys GRYGAR (203 Česká republika) a Oliver HEIRI (756 Švýcarsko)

Vydání

QUATERNARY SCIENCE REVIEWS, KIDLINGTON, OXFORD, ENGLAND, PERGAMON-ELSEVIER SCIENCE LTD, 2016, 0277-3791

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10600 1.6 Biological sciences

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 4.797

Kód RIV

RIV/00216224:14310/16:00088007

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.quascirev.2016.04.001

UT WoS

000376699800008

Klíčová slova česky

Karpaty; klima; rozsivky; geochemie; holocĂ©n; produktivita jezera; pozdnĂÂ glaciĂˇl; pyl; transfer funkce; zmÄ›ny hladiny vody

Klíčová slova anglicky

Carpathians; Climate; Diatoms; Geochemistry; Holocene; Lake-productivity; Late Glacial; Pollen; Transfer functions; Water level changes

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 17. 9. 2020 14:04, doc. RNDr. Petr Pařil, Ph.D.

Anotace

V originále

Temperature reconstructions based on biotic proxies are rare for inland Europe around 49 degrees N. We analysed lake deposits in the Vihorlat Mts in eastern Slovakia. Chironomid head capsules were used to reconstruct mean July temperature (T-July), other proxies (diatoms, green algae, pollen, geochemistry) were used to reconstruct local environmental changes, such as epilimnetic total phosphorus concentrations (TP), lake level changes and development of surrounding vegetation. During the Younger Dryas (YD), temperature fluctuated between 7 and 11 degrees C, that agree with other palaeoclimate records in Europe. The site was somewhat colder than expected from the general south-to-north YD temperature gradient within Europe, possibly because of north-facing exposition. The warmer phases of the YD were characterised by low water level or even complete lake desiccation. At the Late-Glacial/Holocene transition T-July steeply increased from from 11 to 15.5 degrees C - the highest T-July for entire sequence. The open woodlands of conifers and Betula were replaced by broad-leaved temperate forests. At the same time, input of eroded coarse-grained material into the lake decreased and organic matter (LOI) and biogenic silica increased. The Early-Holocene climate was rather stable till 8700 cal yr BP. The lake was productive with a well-developed littoral. A distinct decline of T-July between 8700 and 8000 cal yr BP was associated with decreasing chironomid diversity and increasing climate moistening indicated by pollen. Tychoplanktonic and phosphorus-demanding diatoms increased which might be explained by hydrological and land-cover changes. Later, a gradual warming started after 7000 cal yr BP and representation of macrophytes, periphytic diatoms and littoral chironomids increased. Our results suggest that the Holocene thermal maximum was taking place unusually early in the Holocene at our study site, but its timing might be affected by topography and mesoclimate.

Návaznosti

GAP504/11/0429, projekt VaV

Název: Gradienty prostředí, vegetační dynamika a krajinné změny v Západních Karpatech od pozdního glaciálu po současnost (Akronym: PALAEO-CARPATHIANS)

Investor: Grantová agentura ČR, Environmental gradients, vegetation dynamics and landscape changes in the West Carpathians from the Late Glacial up to the present time

MUNI/A/1048/2015, interní kód MU

Název: Velkoplošná analýza druhové variability evropských biotopů, jejich holocénní vývoj a dynamika (Akronym: VADVEB)

Investor: Masarykova univerzita, Velkoplošná analýza druhové variability evropských biotopů, jejich holocénní vývoj a dynamika, DO R. 2020_Kategorie A - Specifický výzkum - Studentské výzkumné projekty

Přiložené soubory

Hajkova_etal_QSR2016_Hypkana.pdf

Požádat o autorskou verzi souboru

Citovat

HÁJKOVÁ, Petra, Petr PAŘIL, Libor PETR, Barbora CHATTOVÁ, Tomáš Matys GRYGAR a Oliver HEIRI. A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development. QUATERNARY SCIENCE REVIEWS. KIDLINGTON, OXFORD, ENGLAND: PERGAMON-ELSEVIER SCIENCE LTD,, 2016, roč. 141, June, s. 94-111. ISSN 0277-3791. Dostupné z: https://dx.doi.org/10.1016/j.quascirev.2016.04.001.

@article{1348750,
   author = {Hájková, Petra and Pařil, Petr and Petr, Libor and Chattová, Barbora and Grygar, Tomáš Matys and Heiri, Oliver},
   article_location = {KIDLINGTON, OXFORD, ENGLAND},
   article_number = {June},
   doi = {http://dx.doi.org/10.1016/j.quascirev.2016.04.001},
   keywords = {Carpathians; Climate; Diatoms; Geochemistry; Holocene; Lake-productivity; Late Glacial; Pollen; Transfer functions; Water level changes},
   language = {eng},
   issn = {0277-3791},
   journal = {QUATERNARY SCIENCE REVIEWS},
   title = {A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development},
   url = {https://reader.elsevier.com/reader/sd/pii/S0277379116301044?token=B93E8BC910126F0278C47513CAB1A6FF131A352BE5F900CF9D165E3871D3C6BF53D73F66A3869B9B75E3BD90BEA61829},
   volume = {141},
   year = {2016}
}

TY  - JOUR
ID  - 1348750
AU  - Hájková, Petra - Pařil, Petr - Petr, Libor - Chattová, Barbora - Grygar, Tomáš Matys - Heiri, Oliver
PY  - 2016
TI  - A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development
JF  - QUATERNARY SCIENCE REVIEWS
VL  - 141
IS  - June
SP  - 94-111
EP  - 94-111
PB  - PERGAMON-ELSEVIER SCIENCE LTD,
SN  - 02773791
KW  - Carpathians
KW  - Climate
KW  - Diatoms
KW  - Geochemistry
KW  - Holocene
KW  - Lake-productivity
KW  - Late Glacial
KW  - Pollen
KW  - Transfer functions
KW  - Water level changes
UR  - https://reader.elsevier.com/reader/sd/pii/S0277379116301044?token=B93E8BC910126F0278C47513CAB1A6FF131A352BE5F900CF9D165E3871D3C6BF53D73F66A3869B9B75E3BD90BEA61829
L2  - https://reader.elsevier.com/reader/sd/pii/S0277379116301044?token=B93E8BC910126F0278C47513CAB1A6FF131A352BE5F900CF9D165E3871D3C6BF53D73F66A3869B9B75E3BD90BEA61829
N2  - Temperature reconstructions based on biotic proxies are rare for inland Europe around 49 degrees N. We analysed lake deposits in the Vihorlat Mts in eastern Slovakia. Chironomid head capsules were used to reconstruct mean July temperature (T-July), other proxies (diatoms, green algae, pollen, geochemistry) were used to reconstruct local environmental changes, such as epilimnetic total phosphorus concentrations (TP), lake level changes and development of surrounding vegetation. During the Younger Dryas (YD), temperature fluctuated between 7 and 11 degrees C, that agree with other palaeoclimate records in Europe. The site was somewhat colder than expected from the general south-to-north YD temperature gradient within Europe, possibly because of north-facing exposition. The warmer phases of the YD were characterised by low water level or even complete lake desiccation. At the Late-Glacial/Holocene transition T-July steeply increased from from 11 to 15.5 degrees C - the highest T-July for entire sequence. The open woodlands of conifers and Betula were replaced by broad-leaved temperate forests. At the same time, input of eroded coarse-grained material into the lake decreased and organic matter (LOI) and biogenic silica increased. The Early-Holocene climate was rather stable till 8700 cal yr BP. The lake was productive with a well-developed littoral. A distinct decline of T-July between 8700 and 8000 cal yr BP was associated with decreasing chironomid diversity and increasing climate moistening indicated by pollen. Tychoplanktonic and phosphorus-demanding diatoms increased which might be explained by hydrological and land-cover changes. Later, a gradual warming started after 7000 cal yr BP and representation of macrophytes, periphytic diatoms and littoral chironomids increased. Our results suggest that the Holocene thermal maximum was taking place unusually early in the Holocene at our study site, but its timing might be affected by topography and mesoclimate.
ER  -

HÁJKOVÁ, Petra, Petr PAŘIL, Libor PETR, Barbora CHATTOVÁ, Tomáš Matys GRYGAR a Oliver HEIRI. A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development. \textit{QUATERNARY SCIENCE REVIEWS}. KIDLINGTON, OXFORD, ENGLAND: PERGAMON-ELSEVIER SCIENCE LTD,, 2016, roč.~141, June, s.~94-111. ISSN~0277-3791. Dostupné z: https://dx.doi.org/10.1016/j.quascirev.2016.04.001.

Podrobný výpis o publikaci