Description: Oxbow lakes are continuous archives of flood events. On 28th June 2022 a 7.5 m long bottom sediment core (S1: 53.24758°N and 14.46271°E, 2.4 m b.s.l.) was collected from an oxbow lake in the Lower Odra Valley, NW Poland. Drilling was conducted using an Instorf sampler (Russian type; chamber dimension: 10 x 50 cm), onboard a "Manat" catamaran motorboat. After core recovery, each half-metre section was packed into a PVC tube and kept in cool rooms with a constant temperature. Samples were collected every 4 cm. For the first 2 m of the core grain-size, geochemical and Chironomidae analyses as well as radiocarbon dating were performed, which allow to identify flood events in the last 3200 years.
Global identifier:
Doi(
"10.1594/PANGAEA.979942",
)
DataMeasurements(
DataMeasurements {
domain: Unspecified,
station: None,
measured_variables: [
"DEPTH, sediment/rock",
"Dissimilarity, minimum",
"Temperature, air, July, reconstructed",
"Temperature, air, July, reconstructed, standard error",
],
methods: [
"Reconstructed",
],
},
)
Comment: WAPLS_C3_X: Weighted Average Partial Least Squares - Component 3 - X variable C3 indicates the third component or iteration of the PLS analysis X represents the independent variables
Tags: Seen ? Oder ? Lufttemperatur ? Temperatur ? U-Bahn ? Gewässergrund ? Tal ? chironomid composition ? chironomid-inferred temperature reconstructions ?
Bounding boxes: 14.46271° .. 14.46271° x 53.24758° .. 53.24758°
License: cc-by/4.0
Data access requires registration: click here for further informationLanguage: Englisch/English
Modified: 2025-03-25
Time ranges: 2022-06-28 - 2022-06-28
Accessed 1 times.