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Record #191649:

Stratigraphy, sedimentology, age and palaeoenvironment of marine varved clay in the Middle Swedish end-moraine zone / Mark D. Johnson, Ylva Ståhl.

Title: Stratigraphy, sedimentology, age and palaeoenvironment of marine varved clay in the Middle Swedish end-moraine zone / Mark D. Johnson, Ylva Ståhl.
Author(s): Johnson, Mark D.
Ståhl, Ylva.
Date: 2010.
In: Boreas. (2010.), Vol. 39(2) (2010)
Abstract: Examines deposits associated with Middle Swedish end-moraine zone immediately west of Mt. Billingen. Multiple moraine ridges and surrounding inter-moraine flats in study area are underlain by 20-50 m of clay, some of thickest units outside Swedish coastal areas. Reports stratigraphy, sedimentology, age and palaeoenvironment of clay underlying inter-moraine flats. Interprets rhythmites in clay as varves deposited in Arctic marine environment some 12,150 cal. ¹⁴C years ago, i.e., much more recently than moraine ridges formed during ice-front oscillations. Authors neither support nor reject suggestion that ice margin retreated to northern edge of Mt. Billingen during Allerød, causing Baltic Ice Lake to drain.
Notes:

Boreas. Vol. 39(2) :199-214 (2010).

Keywords: 551.33 -- Glacial geology.
551.336 -- Ice ages.
551.324.24 -- Ice sheets and caps.
551.583.3 -- Climatic changes, Quaternary.
551.332.2 -- Drift, glacial. Deposits.
551.324.63 -- Land ice, advance and retreat.
551.332.5 -- Glacial landforms.
551.332.52 -- Moraines, terminal and recessional.
551.791 -- Pleistocene.
550.93 -- Geochronology.
551.332.26 -- Glacio-lacustrine deposits and varves.
E7 -- Glaciology: glacial geology and ice ages.
(*3) -- Arctic regions.
(*57) -- Sweden.
SPRI record no.: 191649

MARCXML

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008 221006s2010####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-191649
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aJohnson, Mark D.
245 10 ‡aStratigraphy, sedimentology, age and palaeoenvironment of marine varved clay in the Middle Swedish end-moraine zone /‡cMark D. Johnson, Ylva Ståhl.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2010.
300 ## ‡ap. 199-214 :‡bill., diags., tables, maps.
500 ## ‡aBoreas. Vol. 39(2) :199-214 (2010).
520 3# ‡aExamines deposits associated with Middle Swedish end-moraine zone immediately west of Mt. Billingen. Multiple moraine ridges and surrounding inter-moraine flats in study area are underlain by 20-50 m of clay, some of thickest units outside Swedish coastal areas. Reports stratigraphy, sedimentology, age and palaeoenvironment of clay underlying inter-moraine flats. Interprets rhythmites in clay as varves deposited in Arctic marine environment some 12,150 cal. ¹⁴C years ago, i.e., much more recently than moraine ridges formed during ice-front oscillations. Authors neither support nor reject suggestion that ice margin retreated to northern edge of Mt. Billingen during Allerød, causing Baltic Ice Lake to drain.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2009.00124.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2009.00124.x
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a551.332.26 -- Glacio-lacustrine deposits and varves.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*57) -- Sweden.‡2udc
700 1# ‡aStåhl, Ylva.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 39(2) (2010) ‡wSPRI-56035
916 ## ‡a2010/08/17 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221006 ‡bRF