Stratigraphic analyses from Lateglacial to late Holocene from sediment core MLC from Moss Lake, Washington, USA

DOI

Magnetic susceptibility was measured at room temperature and low frequency (0.47 kHz) using the MS2C scanner of a Bartington Instruments Ltd MS2 meter to determine allochthonous inputs. The measurements were taken for 10 seconds for each 1 cm section.Organic matter content were estimated via loss-on-ignition (LOI) (heating 550 °C for the organic content)

Identifier
DOI https://doi.org/10.1594/PANGAEA.918529
Related Identifier IsPartOf https://doi.org/10.1594/PANGAEA.918535
Related Identifier IsSupplementTo https://doi.org/10.1007/s10933-022-00244-x
Related Identifier References https://doi.org/10.1594/PANGAEA.890666
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.918529
Provenance
Creator Egan, Joanne ORCID logo; Fletcher, William J ORCID logo; Allott, Timothy E H ORCID logo
Publisher PANGAEA
Publication Year 2020
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 1262 data points
Discipline Earth System Research
Spatial Coverage (-121.847 LON, 47.693 LAT); Moss Lake, Washington, USA