Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment

Ocean-floor sediment samples collected up to 150 years ago represent an important historical archive to benchmark global changes in the seafloor environment, such as species' range shifts and pollution trends. Such benchmarking requires that the historical sediment samples represent the state o...

Full description

Bibliographic Details
Main Authors: Marina Costa Rillo, Michal Kucera, Costa Rillo, Marina
Format: Text
Language:English
Published: Natural History Museum, London 2019
Subjects:
Online Access:https://eprints.soton.ac.uk/448550/
id ftsouthampton:oai:eprints.soton.ac.uk:448550
record_format openpolar
spelling ftsouthampton:oai:eprints.soton.ac.uk:448550 2023-08-27T04:11:36+02:00 Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment Marina Costa Rillo, Michal Kucera Costa Rillo, Marina 2019-01-01 https://eprints.soton.ac.uk/448550/ English eng Natural History Museum, London (2019) Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment. Natural History Museum, London doi:10.5519/0001936 <http://dx.doi.org/10.5519/0001936> [Dataset] Dataset NonPeerReviewed 2019 ftsouthampton https://doi.org/10.5519/0001936 2023-08-03T22:25:13Z Ocean-floor sediment samples collected up to 150 years ago represent an important historical archive to benchmark global changes in the seafloor environment, such as species' range shifts and pollution trends. Such benchmarking requires that the historical sediment samples represent the state of the environment at-or shortly before the time of collection. However, early oceanographic expeditions sampled the ocean floor using devices like the sounding tube or a dredge, which potentially disturb the sediment surface and recover a mix of Holocene (surface) and deeper, Pleistocene sediments. Here we use climate-sensitive microfossils as a fast biometric method to assess if historical seafloor samples contain a mixture of modern and glacial sediments. Our assessment is based on comparing the composition of planktonic foraminifera (PF) assemblages in historical samples with Holocene and Last Glacial Maximum (LGM) global reference datasets. We show that eight out of the nine historical samples contain PF assemblages more similar to the Holocene than to the LGM PF assemblages, but the comparisons are only significant when there is a high local species' temporal turnover (from the LGM to the Holocene). When analysing temporal turnover globally, we show that upwelling and temperate regions had greatest species turnover, which are areas where our methodology would be most diagnostic. Our results suggest that sediment samples from historical collections can provide a baseline of the state of marine ecosystems in the late nineteenth century, and thus be used to assess ocean global change trends. ## Related materials: Rillo MC, Kucera M, Ezard THG and Miller CG (2019) Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment. Front. Mar. Sci. 5:517. doi: https://doi.org/10.3389/fmars.2018.00517 Marina Costa Rillo (2016). Dataset: Henry Buckley Collection of Planktonic Foraminifera. Natural History Museum Data Portal (data.nhm.ac.uk). ... Text Planktonic foraminifera University of Southampton: e-Prints Soton Buckley ENVELOPE(163.933,163.933,-84.967,-84.967)
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Ocean-floor sediment samples collected up to 150 years ago represent an important historical archive to benchmark global changes in the seafloor environment, such as species' range shifts and pollution trends. Such benchmarking requires that the historical sediment samples represent the state of the environment at-or shortly before the time of collection. However, early oceanographic expeditions sampled the ocean floor using devices like the sounding tube or a dredge, which potentially disturb the sediment surface and recover a mix of Holocene (surface) and deeper, Pleistocene sediments. Here we use climate-sensitive microfossils as a fast biometric method to assess if historical seafloor samples contain a mixture of modern and glacial sediments. Our assessment is based on comparing the composition of planktonic foraminifera (PF) assemblages in historical samples with Holocene and Last Glacial Maximum (LGM) global reference datasets. We show that eight out of the nine historical samples contain PF assemblages more similar to the Holocene than to the LGM PF assemblages, but the comparisons are only significant when there is a high local species' temporal turnover (from the LGM to the Holocene). When analysing temporal turnover globally, we show that upwelling and temperate regions had greatest species turnover, which are areas where our methodology would be most diagnostic. Our results suggest that sediment samples from historical collections can provide a baseline of the state of marine ecosystems in the late nineteenth century, and thus be used to assess ocean global change trends. ## Related materials: Rillo MC, Kucera M, Ezard THG and Miller CG (2019) Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment. Front. Mar. Sci. 5:517. doi: https://doi.org/10.3389/fmars.2018.00517 Marina Costa Rillo (2016). Dataset: Henry Buckley Collection of Planktonic Foraminifera. Natural History Museum Data Portal (data.nhm.ac.uk). ...
format Text
author Marina Costa Rillo, Michal Kucera
Costa Rillo, Marina
spellingShingle Marina Costa Rillo, Michal Kucera
Costa Rillo, Marina
Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment
author_facet Marina Costa Rillo, Michal Kucera
Costa Rillo, Marina
author_sort Marina Costa Rillo, Michal Kucera
title Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment
title_short Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment
title_full Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment
title_fullStr Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment
title_full_unstemmed Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment
title_sort supplementary material: surface sediment samples from early age of seafloor exploration can provide a late 19th century baseline of the marine environment
publisher Natural History Museum, London
publishDate 2019
url https://eprints.soton.ac.uk/448550/
long_lat ENVELOPE(163.933,163.933,-84.967,-84.967)
geographic Buckley
geographic_facet Buckley
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation (2019) Supplementary Material: Surface Sediment Samples From Early Age of Seafloor Exploration Can Provide a Late 19th Century Baseline of the Marine Environment. Natural History Museum, London doi:10.5519/0001936 <http://dx.doi.org/10.5519/0001936> [Dataset]
op_doi https://doi.org/10.5519/0001936
_version_ 1775354537058500608