Midlands State University Library

How cold was the Little Ice Age? A proxy-based reconstruction from Finland applying modern analogues of fossil midge assemblages (Record no. 161854)

MARC details
000 -LEADER
fixed length control field 02104nam a22002417a 4500
003 - CONTROL NUMBER IDENTIFIER
control field ZW-GwMSU
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20230424094323.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 230413b |||||||| |||| 00| 0 eng d
040 ## - CATALOGING SOURCE
Original cataloging agency MSU
Transcribing agency MSU
Description conventions rda
100 ## - MAIN ENTRY--PERSONAL NAME
Personal name LUOTO, Tomi P.
245 ## - TITLE STATEMENT
Title How cold was the Little Ice Age? A proxy-based reconstruction from Finland applying modern analogues of fossil midge assemblages
264 ## - PRODUCTION, PUBLICATION, DISTRIBUTION, MANUFACTURE, AND COPYRIGHT NOTICE
Place of production, publication, distribution, manufacture Verlag
Name of producer, publisher, distributor, manufacturer Springer
Date of production, publication, distribution, manufacture, or copyright notice 2013
336 ## - CONTENT TYPE
Source rdacontent
Content type term text
Content type code txt
337 ## - MEDIA TYPE
Source rdamedia
Media type term unmediated
Media type code n
338 ## - CARRIER TYPE
Source rdacarrier
Carrier type term volume
Carrier type code nc
440 ## - SERIES STATEMENT/ADDED ENTRY--TITLE
Title Environmental earth sciences
Volume/sequential designation Volume , number ,
520 ## - SUMMARY, ETC.
Summary, etc. Climate dynamics during the past ca. 700 years in southern Finland were reconstructed using fossil midge (Diptera:Nematocera) assemblages aiming to estimate quantitatively the temperature change that has occurred from the Little Ice Age to the present. Midge stratigraphies of two sediment cores from eastern and southern Finland were chosen to be examined for temperature inferences utilizing the modern analogue technique. The new midge-based temperature inference model had a coefficient of determination of 0.901 and a prediction error of 0.498 °C, showing improvement over the previous Finnish models. The combined curve of the inferred temperatures derived from both of the cores showed a decrease towards ca. 1700 AD, when temperatures were approximately 1 °C cooler than the past 700 years average and almost 2 °C colder than present. The temperatures began to increase in southern Finland from 1800 AD and in eastern Finland from 1900 AD onwards. The highest temperatures were reached at the top of the core, representing the present climate warming. Although there was slight overestimation in the recent inferred values, the reconstructed trends were in close correspondence with the previous proxy-based, historical, and measured data that suggests that the reconstruction was realistic and reliable.
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element modern analogue technique
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element little ice age
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element climate change
856 ## - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier https://doi.org/10.1007/s12665-012-1830-9
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme Library of Congress Classification
Koha item type Journal Article
Holdings
Withdrawn status Lost status Source of classification or shelving scheme Damaged status Not for loan Home library Current library Shelving location Date acquired Serial Enumeration / chronology Total Checkouts Full call number Date last seen Price effective from Koha item type Public note
    Library of Congress Classification     Main Library Main Library - Special Collections 24/04/2023 Vol.68 , No.5 (Marc 2013)   GE105 ENV 24/04/2023 24/04/2023 Journal Article For In House Use Only