Paper · 1959 · Philosophical transactions of the Royal Society of London. Series B, Biological sciences

Studies in the Post-glacial history of British vegetation XIV. Late-glacial deposits at Moss Lake, Liverpool

Harry Godwin

7
claims
10
verbatim quotes
27
citations
2
research areas
—
Not open access

Abstract

Abstract Investigations of deposits at a built-over site near the centre of Liverpool disclose a basal stratigraphic sequence characteristic of the west-European Late-glacial period. Detailed pollen analyses confirm that the deposits extended from the Late-glacial (Zone I) to the Post-glacial thermal maximum (Zone VII a). The lake was overgrown in Zone VI by floating sphagna , and in Zone VII a typical raised bog developed. Macroscopic remains of lake and fen plants were recovered in great abundance and together with frequent non-tree pollen these permitted a detailed reconstruction of the vegetational history of both the lake and the surrounding upland. Several species of notably disjunct or restricted present-day range have been recorded here, Cotoneaster cf. integerrima Medic., Elatine hexandra (Lapierre) D.C., Lycopodium annotinum L., Pilularia globulifera L., and Linum anglicum Mill., whilst tentative identification of species such as Agropyron junceiforme, A. & D. Löve, Gentiana campestris (L.), Lotus uliginosus Schkuhr, and Vicia sepium L. cast new light on the natural status of other British plants. Numerous further records confirm and extend our knowledge of the history of the British flora, especially in the Late-glacial and early Post-glacial periods.

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Claims 7

Observationobservedoriginal resultmeasured

Claim · model-written summary

Deposits near central Liverpool contained a basal stratigraphic sequence characteristic of the west-European Late-glacial.

Taxon
British vegetationt0
Outcome
basal stratigraphic sequence characteristic of the west-European Late-glacial periode0
Setting
Liverpoole0

Verbatim

e0

“Investigations of deposits at a built-over site near the centre of Liverpool disclose a basal stratigraphic sequence characteristic of the west-European Late-glacial period.”

✓ located verbatim in the source · abstract, characters 9–182 · show in text ↑
t0

“British vegetation”

✓ located verbatim in the source · title, characters 39–57 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

Pollen analysis dated the deposits from Zone I to Zone VII a.

Taxon
British vegetationt0
Outcome
deposits extended from the Late-glacial (Zone I) to the Post-glacial thermal maximum (Zone VII a)e0

Verbatim

e0

“Detailed pollen analyses confirm that the deposits extended from the Late-glacial (Zone I) to the Post-glacial thermal maximum (Zone VII a).”

✓ located verbatim in the source · abstract, characters 183–323 · show in text ↑
t0

“British vegetation”

✓ located verbatim in the source · title, characters 39–57 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

Floating sphagna overgrew the lake in Zone VI.

Taxon
floating sphagnae0
Outcome
lake was overgrown in Zone VIe0

Verbatim

e0

“The lake was overgrown in Zone VI by floating sphagna , and in Zone VII a typical raised bog developed.”

✓ located verbatim in the source · abstract, characters 324–427 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

A typical raised bog developed in Zone VII a.

Taxon
British vegetationt0
Outcome
typical raised bog developede0

Verbatim

e0

“The lake was overgrown in Zone VI by floating sphagna , and in Zone VII a typical raised bog developed.”

✓ located verbatim in the source · abstract, characters 324–427 · show in text ↑
t0

“British vegetation”

✓ located verbatim in the source · title, characters 39–57 · show in text ↑
Method / resourceobservedoriginal resultmeasured

Claim · model-written summary

Abundant lake and fen plant remains and non-tree pollen enabled reconstruction of lake and upland vegetation history.

Taxon
lake and fen plantse0
Outcome
detailed reconstruction of the vegetational history of both the lake and the surrounding uplande0
Value
great abundancee0

Verbatim

e0

“Macroscopic remains of lake and fen plants were recovered in great abundance and together with frequent non-tree pollen these permitted a detailed reconstruction of the vegetational history of both the lake and the surrounding upland.”

✓ located verbatim in the source · abstract, characters 428–662 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

Cotoneaster cf. integerrima Medic., Elatine hexandra and Lycopodium annotinum were recorded at the site despite restricted or disjunct present ranges.

Taxon
Cotoneaster cf. integerrima Medic.e0
Outcome
have been recorded heree0

Verbatim

e0

“Several species of notably disjunct or restricted present-day range have been recorded here, Cotoneaster cf. integerrima Medic., Elatine hexandra (Lapierre) D.C., Lycopodium annotinum L., Pilularia globulifera L., and Linum anglicum Mill.”

✓ located verbatim in the source · abstract, characters 663–901 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

Pilularia globulifera and Linum anglicum were recorded at the site despite restricted or disjunct present ranges.

Taxon
Pilularia globulifera L.Pilularia globuliferae0
Outcome
have been recorded heree0

Organisms pictured · Representative pictures of the matched species, not figures from the paper.

Pilularia globulifera
Pilularia globulifera · TaxonDysmorodrepanis · CC BY-SA 3.0 · Wikimedia Commons ↗

Verbatim

e0

“Several species of notably disjunct or restricted present-day range have been recorded here, Cotoneaster cf. integerrima Medic., Elatine hexandra (Lapierre) D.C., Lycopodium annotinum L., Pilularia globulifera L., and Linum anglicum Mill.”

✓ located verbatim in the source · abstract, characters 663–901 · show in text ↑