_version_ 1867170141184196608
author Antczak-Orlewska, Olga
Święta-Musznicka, Joanna
Trębska, Gabriela
Janik, Ewa
Rzodkiewicz, Monika
Pawłowski, Dominik
Okupny, Daniel
Nazarova, Larisa B
Kuliński, Karol
Koziorowska, Katarzyna
Kittel, Piotr
Kotrys, Bartosz
Płóciennik, Mateusz
author_facet Antczak-Orlewska, Olga
Święta-Musznicka, Joanna
Trębska, Gabriela
Janik, Ewa
Rzodkiewicz, Monika
Pawłowski, Dominik
Okupny, Daniel
Nazarova, Larisa B
Kuliński, Karol
Koziorowska, Katarzyna
Kittel, Piotr
Kotrys, Bartosz
Płóciennik, Mateusz
collection Datos científicos de ciencias marinas y ambientales
contents This data set presents the reconstructed water level for AL1 sediment core based on subfossil Chironomidae data. The core was collected in July 2019 from from the lower alas level, approximately 1.5 km north of the Berelekh River (70.84057° N, 147.48369° E). It was taken from the active layer as a monolith using a Russian auger and was subsequently cut into 1-cm slices in the laboratory of the Chokurdakh Scientific Tundra Station. Water depth was reconstructed using the East-Siberian chironomid-based inference model (WA-PLS, 1 component; r2 boot = 0.62; RMSEP = 0.35) based on a modern calibration dataset of 150 lakes from Yakutia (Nazarova et al., 2011). To determine whether the modern calibration model had adequate analogues for the fossil assemblages, the modern analogue technique (MAT) was performed using C2 version 1.7.7 (Juggins, 2007) on percentage, square-root-transformed data. The distance between each fossil sample and its most similar modern assemblage was compared, and the 5th percentile of all squared-chord distances of the modern data was used to define the cut-off for a good analogue (Plikk et al., 2019).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_987967
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Chironomidae-inferred late Holocene water level reconstruction from the alas lake (AL1 profile) in the Yana-Indigirka Lowland, NE Yakutia
Antczak-Orlewska, Olga
Święta-Musznicka, Joanna
Trębska, Gabriela
Janik, Ewa
Rzodkiewicz, Monika
Pawłowski, Dominik
Okupny, Daniel
Nazarova, Larisa B
Kuliński, Karol
Koziorowska, Katarzyna
Kittel, Piotr
Kotrys, Bartosz
Płóciennik, Mateusz
Alas; Arctic; Bootstrapping cross validation, standard error; Chironomidae; DEPTH, sediment/rock; Dissimilarity, minimum; HOLARCLIM_AL1; Lake, water depth, reconstructed; Northeast Yakutia, Russia; Palaeoecology; reconstruction; Russian auger; Standard deviation; thermokarst lake; Transfer function; weighted averaging partial least squares (WA-PLS); tundra zone; water level; wetland
This data set presents the reconstructed water level for AL1 sediment core based on subfossil Chironomidae data. The core was collected in July 2019 from from the lower alas level, approximately 1.5 km north of the Berelekh River (70.84057° N, 147.48369° E). It was taken from the active layer as a monolith using a Russian auger and was subsequently cut into 1-cm slices in the laboratory of the Chokurdakh Scientific Tundra Station. Water depth was reconstructed using the East-Siberian chironomid-based inference model (WA-PLS, 1 component; r2 boot = 0.62; RMSEP = 0.35) based on a modern calibration dataset of 150 lakes from Yakutia (Nazarova et al., 2011). To determine whether the modern calibration model had adequate analogues for the fossil assemblages, the modern analogue technique (MAT) was performed using C2 version 1.7.7 (Juggins, 2007) on percentage, square-root-transformed data. The distance between each fossil sample and its most similar modern assemblage was compared, and the 5th percentile of all squared-chord distances of the modern data was used to define the cut-off for a good analogue (Plikk et al., 2019).
title Chironomidae-inferred late Holocene water level reconstruction from the alas lake (AL1 profile) in the Yana-Indigirka Lowland, NE Yakutia
topic Alas; Arctic; Bootstrapping cross validation, standard error; Chironomidae; DEPTH, sediment/rock; Dissimilarity, minimum; HOLARCLIM_AL1; Lake, water depth, reconstructed; Northeast Yakutia, Russia; Palaeoecology; reconstruction; Russian auger; Standard deviation; thermokarst lake; Transfer function; weighted averaging partial least squares (WA-PLS); tundra zone; water level; wetland
url https://doi.org/10.1594/PANGAEA.987967