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Record #172250:

Comsmogenic ¹⁰Be ages on the Pomeranian Moraine, Poland / Vincent R. Rinterknech, and 6 others.

Title: Comsmogenic ¹⁰Be ages on the Pomeranian Moraine, Poland / Vincent R. Rinterknech, and 6 others.
Author(s): Rinterknech, Vincent R.
Date: 2005.
In: Boreas. (2005.), Vol. 34(2) (2005)
Abstract: Presents 37 ¹⁰Be ages that provide first direct dating of Pomeranian Moraine, a prominent recessional moraine deposited in northern Poland following last maximum extent of Scandinavian ice sheet (SIS). Describes setting, sampling strategy and methodology, discussing corrections for uplift, topographic shielding, vegetation and intermittent snow cover. Results indicate mean age of 14.8 ± 0.4 ¹⁰Be ka for final deposition of moraine, suggesting southern margin of SIS was near maximum extent later than previously inferred, with retreat probably occurring in response to onset of Bølling interstade.
Notes:

Boreas. Vol. 34(2) :186-191 (2005).

Keywords: 551.33 -- Glacial geology.
551.337 -- Chronology of the Pleistocene and recent periods.
550.93 -- Geochronology.
546.45 -- Beryllium.
551.324.24 -- Ice sheets and caps: Scandinavian ice sheet.
551.332.52 -- Moraines, terminal and recessional.
551.241 -- Plate tectonics.
551.578.46 -- Snow cover and snow patches.
551.324.6 -- Land ice, fluctuation.
E7 -- Glaciology: glacial geology and ice ages.
(438) -- Poland.
SPRI record no.: 172250

MARCXML

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035 ## ‡aSPRI-172250
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100 1# ‡aRinterknech, Vincent R.
245 10 ‡aComsmogenic ¹⁰Be ages on the Pomeranian Moraine, Poland /‡cVincent R. Rinterknech, and 6 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2005.
300 ## ‡ap. 186-191 :‡bdiags., table, map.
500 ## ‡aBoreas. Vol. 34(2) :186-191 (2005).
520 3# ‡aPresents 37 ¹⁰Be ages that provide first direct dating of Pomeranian Moraine, a prominent recessional moraine deposited in northern Poland following last maximum extent of Scandinavian ice sheet (SIS). Describes setting, sampling strategy and methodology, discussing corrections for uplift, topographic shielding, vegetation and intermittent snow cover. Results indicate mean age of 14.8 ± 0.4 ¹⁰Be ka for final deposition of moraine, suggesting southern margin of SIS was near maximum extent later than previously inferred, with retreat probably occurring in response to onset of Bølling interstade.
530 ## ‡aAlso issued online ‡uurn:doi:10.1080/03009480510012926‡uhttps://dx.doi.org/10.1080/03009480510012926
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a546.45 -- Beryllium.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps: Scandinavian ice sheet.‡2udc
650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc
650 07 ‡a551.241 -- Plate tectonics.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(438) -- Poland.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 34(2) (2005) ‡wSPRI-56035
916 ## ‡a2005/06/07 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221006 ‡bRF