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Record #191607:

The omission of conflicting evidence from the paper by Golledge et al. (2008) / Derek Flinn.

Title: The omission of conflicting evidence from the paper by Golledge et al. (2008) / Derek Flinn.
Author(s): Flinn, Derek.
Date: 2009.
In: Geografiska Annaler. Series A. Physical Geography. (2009.), Vol. 91(4) (2009)
Abstract: Criticises paper The last glaciation of Shetland, North Atlantic. Geografiska Annaler, 90 A(1): 37-53, which concluded on basis of remote sensing study that islands were overrun by ice from Scandinavia during last glacial maximum in Shetland. Argues that paper's method did not reveal direction of ice flow and that authors ignored earlier ground-based work on striations that did, leaving their conclusions without scientific basis. Presents and discusses published evidence (including Flinn's own) from striation mapping. Does not argue that Shetlands were not overrun by Scandinavian ice at this time, only that omission of all evidence suggesting contrary renders paper unscientific.
Notes:

Geografiska Annaler. Series A. Physical Geography. Vol. 91(4) :253-256 (2009).

Keywords: 551.33 -- Glacial geology.
551.324 -- Land ice.
551.336 -- Ice ages.
551.324.24 -- Ice sheets and caps: Scandinavian Ice Sheet.
551.324.54 -- Land ice, flow of particular glaciers.
551.331.5 -- Glacial erosion and protection. Sub-glacial topography.
551.331.55 -- Rock, polished, grooved and striated by glacial action.
528.9 -- Cartography.
53.087.23 -- Remote sensing.
E7 -- Glaciology: glacial geology and ice ages.
(411) -- Scotland.
SPRI record no.: 191607

MARCXML

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100 1# ‡aFlinn, Derek.
245 14 ‡aThe omission of conflicting evidence from the paper by Golledge et al. (2008) /‡cDerek Flinn.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 253-256 :‡bill., diag., map.
500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 91(4) :253-256 (2009).
520 3# ‡aCriticises paper The last glaciation of Shetland, North Atlantic. Geografiska Annaler, 90 A(1): 37-53, which concluded on basis of remote sensing study that islands were overrun by ice from Scandinavia during last glacial maximum in Shetland. Argues that paper's method did not reveal direction of ice flow and that authors ignored earlier ground-based work on striations that did, leaving their conclusions without scientific basis. Presents and discusses published evidence (including Flinn's own) from striation mapping. Does not argue that Shetlands were not overrun by Scandinavian ice at this time, only that omission of all evidence suggesting contrary renders paper unscientific.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps: Scandinavian Ice Sheet.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers.‡2udc
650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc
650 07 ‡a551.331.55 -- Rock, polished, grooved and striated by glacial action.‡2udc
650 07 ‡a528.9 -- Cartography.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(411) -- Scotland.‡2udc
773 0# ‡7nnas ‡tGeografiska Annaler. Series A. Physical Geography. ‡gVol. 91(4) (2009) ‡wSPRI-40621
916 ## ‡a2010/06/30 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929 ‡bRF