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The Holocene (source)
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Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications
Latalowa, Malgorzata
;
Swięta-Musznicka, Joanna
;
Słowinski, Michal
;
Stivrinš, Normunds
The Holocene
2019
/
p. 1335-1349 : ill
https://doi.org/10.1177/0959683619846978
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journal article ENG
2
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journal article ENG
Integrating fire-scar, charcoal and fungal spore data to study fire events in the boreal forest of northern Europe
Stivrinš, Normunds
The Holocene
2019
/
11 p. : ill
https://doi.org/10.1177/0959683619854524
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journal article ENG
3
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journal article ENG
Palaeoenvironmental evidence for the impact of the crusades on the local and regional environment of medieval (13th-16th century) northern Latvia, eastern Baltic
Stivrinš, Normunds
;
Brown, Alex
;
Veski, Siim
;
Ratniece, Vita
;
Heinsalu, Atko
;
Austin, Jennifer
;
Liiv, Merlin
;
Cerina, Aija
The Holocene
2016
/
p. 61-69 : ill
https://doi.org/10.1177/0959683615596821
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4
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journal article ENG
Postglacial flooding and vegetation history on the Ob River terrace, central Western Siberia based on the palaeoecological record from Lake Svetlenkoye
Amon, Leeli
;
Blaus, Ansis
;
Alliksaar, Tiiu
;
Heinsalu, Atko
;
Lapshina, Elena
;
Liiv, Merlin
;
Reitalu, Triin
;
Vassiljev, Jüri
;
Veski, Siim
The Holocene
2020
/
p. 618–631
https://doi.org/10.1177/0959683619895582
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5
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journal article ENG
Sea level changes and Neolithic hunter-fisher-gatherers in the centre of Tallinn, southern coast of the Gulf of Finland, Baltic Sea
Muru, Merle
;
Rosentau, Alar
;
Kriiska, Aivar
;
Vassiljev, Jüri
;
Saarse, Leili
The Holocene
2017
/
p. 917-928 : ill
https://doi.org/10.1177/0959683616678462
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6
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The final meltdown of dead-ice at the Holocene Thermal Maximum (8500–7400 cal. yr BP) in western Latvia, eastern Baltic
Stivrinš, Normunds
;
Liiv, Merlin
;
Heinsalu, Atko
;
Galka, Mariusz
;
Veski, Siim
The Holocene
2017
/
p. 1146-1157 : ill
https://doi.org/10.1177/0959683616683255
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journal article ENG
Number of records 6, displaying
1 - 6
keyword
3
1.
holocene thermal maximum
2.
Early Holocene
3.
holocene
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