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Record #214390:
Late Holocene high precipitation events recorded in lake sediments and catchment geomorphology, Lake Vuoksjávrátje, NW Sweden / Annika Berntsson, and 4 others.
Title: | Late Holocene high precipitation events recorded in lake sediments and catchment geomorphology, Lake Vuoksjávrátje, NW Sweden / Annika Berntsson, and 4 others. |
Author(s): | Berntsson, Annika. |
Date: | 2015. |
In: | Boreas. (2015.), Vol. 44(4) (2015) |
Abstract: | Demonstrates potential of combining analysis of abiotic and biotic proxies with catchment geomorphology to improve understanding of climate and environmental change in Late Holocene. Results indicate relatively stable climate conditions from commencement of records 5100 years ago until c. 2900 cal. yr BP. Then, record displays increasingly variable sediment input, interpreted as result of intense precipitation events. |
Notes: | Boreas. Vol. 44(4) :676-692 (2015). |
Keywords: | 551.4 -- Geomorphology. 551.577 -- Precipitation. 551.583 -- Climatic changes. 551.583.3 -- Climatic changes, Quaternary. 551.794 -- Holocene. 556 -- Hydrology. 556.55 -- Lakes and ponds. 551.8 -- Palaeogeography. 556.555.6 -- Lakes, sediments. 574 -- Ecology. 56 -- Palaeontology. D -- Atmospheric sciences. (*3) -- Arctic regions. (*57) -- Sweden. |
SPRI record no.: | 214390 |
LDR 01732naa#a2200000#a#4500 001 SPRI-214390 005 20230925151622.0 007 ta 008 230925s2015####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-214390 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBerntsson, Annika. 245 10 ‡aLate Holocene high precipitation events recorded in lake sediments and catchment geomorphology, Lake Vuoksjávrátje, NW Sweden /‡cAnnika Berntsson, and 4 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2015. 300 ## ‡ap. 676-692 :‡bill., diags., tables, maps. 500 ## ‡aBoreas. Vol. 44(4) :676-692 (2015). 520 3# ‡aDemonstrates potential of combining analysis of abiotic and biotic proxies with catchment geomorphology to improve understanding of climate and environmental change in Late Holocene. Results indicate relatively stable climate conditions from commencement of records 5100 years ago until c. 2900 cal. yr BP. Then, record displays increasingly variable sediment input, interpreted as result of intense precipitation events. 530 ## ‡aAlso issued online ‡uurn:doi:10.1111/bor.12127‡uhttps://dx.doi.org/10.1111/bor.12127 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡a551.577 -- Precipitation.‡2udc 650 07 ‡a551.583 -- Climatic changes.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a551.794 -- Holocene.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡a556.55 -- Lakes and ponds.‡2udc 650 07 ‡a551.8 -- Palaeogeography.‡2udc 650 07 ‡a556.555.6 -- Lakes, sediments.‡2udc 650 07 ‡a574 -- Ecology.‡2udc 650 07 ‡a56 -- Palaeontology.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*57) -- Sweden.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 44(4) (2015) ‡wSPRI-56035 916 ## ‡a2015/10/29 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230925 ‡bJW ‡dPGA