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...

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Main Author: Marina Costa Rillo, Michal Kucera, Thomas H. G. Ezard, C. Giles Miller
Format: Dataset
Language:English
Published: Natural History Museum 2019
Subjects:
Online Access:https://dx.doi.org/10.5519/0001936
http://data.nhm.ac.uk/dataset/a79a684f-fc60-4348-b619-34d61b3b31da
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spelling ftdatacite:10.5519/0001936 2023-05-15T18:00:44+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, Thomas H. G. Ezard, C. Giles Miller 2019 CSV https://dx.doi.org/10.5519/0001936 http://data.nhm.ac.uk/dataset/a79a684f-fc60-4348-b619-34d61b3b31da en eng Natural History Museum dataset Research Dataset 2019 ftdatacite https://doi.org/10.5519/0001936 2021-11-05T12:55:41Z 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). https://doi.org/10.5519/0035055 Dataset Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Buckley ENVELOPE(163.933,163.933,-84.967,-84.967)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
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). https://doi.org/10.5519/0035055
format Dataset
author Marina Costa Rillo, Michal Kucera, Thomas H. G. Ezard, C. Giles Miller
spellingShingle Marina Costa Rillo, Michal Kucera, Thomas H. G. Ezard, C. Giles Miller
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, Thomas H. G. Ezard, C. Giles Miller
author_sort Marina Costa Rillo, Michal Kucera, Thomas H. G. Ezard, C. Giles Miller
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
publishDate 2019
url https://dx.doi.org/10.5519/0001936
http://data.nhm.ac.uk/dataset/a79a684f-fc60-4348-b619-34d61b3b31da
long_lat ENVELOPE(163.933,163.933,-84.967,-84.967)
geographic Buckley
geographic_facet Buckley
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_doi https://doi.org/10.5519/0001936
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