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 |