In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 50, No. 8 ( 2023-04-28)
Abstract:
The loess 10 Be‐derived M‐G boundary is located in paleosol S 32 (corresponding to MIS 103), consistent with marine sediment records The age of the 10 Be‐derived M‐G boundary is ∼19 ka younger than the age of paleomagnetic measurements in the same loess sediments The primary magnetic remanence obtained during the M‐G polarity reversal was overprinted by later superimposed magnetic signals
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2022GL102486
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2023
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13