Large-scale magmatic pulses drive plant ecosystem dynamics

The 6.6 km gross thickness of the Palaeogene lava field of the Faroe Islands Basalt Group was erupted in the initial phases of North Atlantic rifting. Thin interlava sedimentary rocks yield palynofloras that vary in composition and diversity with the duration of the interlava period. Long-term trend...

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Bibliographic Details
Main Authors: David W. Jolley, Simon R. Passey, Malcolm Hole, John Millett
Format: Dataset
Language:unknown
Published: 2016
Subjects:
TiO
6.6
MgO
km
Online Access:https://doi.org/10.6084/m9.figshare.3453095.v1
https://figshare.com/articles/Large-scale_magmatic_pulses_drive_plant_ecosystem_dynamics/3453095
id ftgeosoclonfig:oai:figshare.com:article/3453095
record_format openpolar
spelling ftgeosoclonfig:oai:figshare.com:article/3453095 2023-05-15T16:10:32+02:00 Large-scale magmatic pulses drive plant ecosystem dynamics David W. Jolley Simon R. Passey Malcolm Hole John Millett 2016-06-21T11:08:03Z https://doi.org/10.6084/m9.figshare.3453095.v1 https://figshare.com/articles/Large-scale_magmatic_pulses_drive_plant_ecosystem_dynamics/3453095 unknown doi:10.6084/m9.figshare.3453095.v1 https://figshare.com/articles/Large-scale_magmatic_pulses_drive_plant_ecosystem_dynamics/3453095 CC BY 4.0 CC-BY Geology magmatic trend pulse eruption tempo Palaeogene lava field Faroe Islands Basalt Group duration disturbance thickness palynoflora TiO interlava 6.6 MgO diversity North Atlantic rifting basalt lava flows show Thin phase vegetation ecosystem dynamics substrate km fractionation succession Dataset 2016 ftgeosoclonfig https://doi.org/10.6084/m9.figshare.3453095.v1 2020-02-21T07:24:30Z The 6.6 km gross thickness of the Palaeogene lava field of the Faroe Islands Basalt Group was erupted in the initial phases of North Atlantic rifting. Thin interlava sedimentary rocks yield palynofloras that vary in composition and diversity with the duration of the interlava period. Long-term trends in plant ecological succession occur within the record, each reflecting initially rapid and subsequently slowing eruption tempo. TiO 2 and MgO plots derived from the basalt lava flows show corresponding fractionation trends. These link melt column processes to vegetation ecosystem dynamics via controls on eruption tempo, thermal support and substrate disturbance. Dataset Faroe Islands North Atlantic Geological Society of London: Figshare Faroe Islands
institution Open Polar
collection Geological Society of London: Figshare
op_collection_id ftgeosoclonfig
language unknown
topic Geology
magmatic
trend
pulse
eruption tempo
Palaeogene lava field
Faroe Islands Basalt Group
duration
disturbance
thickness
palynoflora
TiO
interlava
6.6
MgO
diversity
North Atlantic rifting
basalt lava flows show
Thin
phase
vegetation ecosystem dynamics
substrate
km
fractionation
succession
spellingShingle Geology
magmatic
trend
pulse
eruption tempo
Palaeogene lava field
Faroe Islands Basalt Group
duration
disturbance
thickness
palynoflora
TiO
interlava
6.6
MgO
diversity
North Atlantic rifting
basalt lava flows show
Thin
phase
vegetation ecosystem dynamics
substrate
km
fractionation
succession
David W. Jolley
Simon R. Passey
Malcolm Hole
John Millett
Large-scale magmatic pulses drive plant ecosystem dynamics
topic_facet Geology
magmatic
trend
pulse
eruption tempo
Palaeogene lava field
Faroe Islands Basalt Group
duration
disturbance
thickness
palynoflora
TiO
interlava
6.6
MgO
diversity
North Atlantic rifting
basalt lava flows show
Thin
phase
vegetation ecosystem dynamics
substrate
km
fractionation
succession
description The 6.6 km gross thickness of the Palaeogene lava field of the Faroe Islands Basalt Group was erupted in the initial phases of North Atlantic rifting. Thin interlava sedimentary rocks yield palynofloras that vary in composition and diversity with the duration of the interlava period. Long-term trends in plant ecological succession occur within the record, each reflecting initially rapid and subsequently slowing eruption tempo. TiO 2 and MgO plots derived from the basalt lava flows show corresponding fractionation trends. These link melt column processes to vegetation ecosystem dynamics via controls on eruption tempo, thermal support and substrate disturbance.
format Dataset
author David W. Jolley
Simon R. Passey
Malcolm Hole
John Millett
author_facet David W. Jolley
Simon R. Passey
Malcolm Hole
John Millett
author_sort David W. Jolley
title Large-scale magmatic pulses drive plant ecosystem dynamics
title_short Large-scale magmatic pulses drive plant ecosystem dynamics
title_full Large-scale magmatic pulses drive plant ecosystem dynamics
title_fullStr Large-scale magmatic pulses drive plant ecosystem dynamics
title_full_unstemmed Large-scale magmatic pulses drive plant ecosystem dynamics
title_sort large-scale magmatic pulses drive plant ecosystem dynamics
publishDate 2016
url https://doi.org/10.6084/m9.figshare.3453095.v1
https://figshare.com/articles/Large-scale_magmatic_pulses_drive_plant_ecosystem_dynamics/3453095
geographic Faroe Islands
geographic_facet Faroe Islands
genre Faroe Islands
North Atlantic
genre_facet Faroe Islands
North Atlantic
op_relation doi:10.6084/m9.figshare.3453095.v1
https://figshare.com/articles/Large-scale_magmatic_pulses_drive_plant_ecosystem_dynamics/3453095
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.3453095.v1
_version_ 1765995719182778368