History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene

How will freshwater lakes in the Arctic respond to climate change, especially if polar amplification results in even greater warming at these northern latitudes? Deep time analogs offer opportunities to understand the potential effects of future climate warming on arctic environments. A core from th...

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Published in:Journal of Paleontology
Main Authors: Peter A. Siver, Anne Marie Lott
Format: Text
Language:English
Published: The Paleontological Society 2023
Subjects:
Online Access:https://doi.org/10.1017/jpa.2022.101
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spelling ftbioone:10.1017/jpa.2022.101 2024-06-02T08:01:05+00:00 History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene Peter A. Siver Anne Marie Lott Peter A. Siver Anne Marie Lott world 2023-04-11 text/HTML https://doi.org/10.1017/jpa.2022.101 en eng The Paleontological Society doi:10.1017/jpa.2022.101 All rights reserved. https://doi.org/10.1017/jpa.2022.101 Text 2023 ftbioone https://doi.org/10.1017/jpa.2022.101 2024-05-07T00:48:07Z How will freshwater lakes in the Arctic respond to climate change, especially if polar amplification results in even greater warming at these northern latitudes? Deep time analogs offer opportunities to understand the potential effects of future climate warming on arctic environments. A core from the Giraffe Pipe fossil locality located in the Northwest Territories of Canada offers a window into the life of a thriving Arctic freshwater ecosystem in the Eocene during greenhouse conditions. The remains of an extensive deposit of microfossils, including photosynthetic protists (chrysophytes, diatoms, and green algae), heterotrophic protists (euglyphids, heliozoans, paraphysomonads, and rotosphaerids), and sponges, were used to reconstruct the history of the ancient waterbody. Concentrations and diversity of chrysophyte taxa were extensive throughout the core, accounting for >70% of the microfossil remains. The ratio of chrysophyte cysts to diatom valves, with a mean value near 14 throughout the core, further emphasized the dominance of the chrysophytes, and given the high diversity of taxa, the locality represents a “paleo-hotspot” for this eukaryote lineage. Based on the totality of fossil evidence, the waterbody within the Giraffe Pipe crater represented a series of relatively shallow aquatic habitats, with changing physical and chemical conditions, and varying water depths. Five major zones were identified, each found to be stable for an extended period of time, but with distinct transitions between successive zones signaling significant shifts in environmental conditions. The study provides valuable insight on how Arctic freshwater ecosystems responded to past warm climates, and to the organisms that could potentially thrive in these environments under future warming scenarios. Text Arctic Climate change Northwest Territories BioOne Online Journals Arctic Canada Northwest Territories Journal of Paleontology 97 2 271 291
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description How will freshwater lakes in the Arctic respond to climate change, especially if polar amplification results in even greater warming at these northern latitudes? Deep time analogs offer opportunities to understand the potential effects of future climate warming on arctic environments. A core from the Giraffe Pipe fossil locality located in the Northwest Territories of Canada offers a window into the life of a thriving Arctic freshwater ecosystem in the Eocene during greenhouse conditions. The remains of an extensive deposit of microfossils, including photosynthetic protists (chrysophytes, diatoms, and green algae), heterotrophic protists (euglyphids, heliozoans, paraphysomonads, and rotosphaerids), and sponges, were used to reconstruct the history of the ancient waterbody. Concentrations and diversity of chrysophyte taxa were extensive throughout the core, accounting for >70% of the microfossil remains. The ratio of chrysophyte cysts to diatom valves, with a mean value near 14 throughout the core, further emphasized the dominance of the chrysophytes, and given the high diversity of taxa, the locality represents a “paleo-hotspot” for this eukaryote lineage. Based on the totality of fossil evidence, the waterbody within the Giraffe Pipe crater represented a series of relatively shallow aquatic habitats, with changing physical and chemical conditions, and varying water depths. Five major zones were identified, each found to be stable for an extended period of time, but with distinct transitions between successive zones signaling significant shifts in environmental conditions. The study provides valuable insight on how Arctic freshwater ecosystems responded to past warm climates, and to the organisms that could potentially thrive in these environments under future warming scenarios.
author2 Peter A. Siver
Anne Marie Lott
format Text
author Peter A. Siver
Anne Marie Lott
spellingShingle Peter A. Siver
Anne Marie Lott
History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene
author_facet Peter A. Siver
Anne Marie Lott
author_sort Peter A. Siver
title History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene
title_short History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene
title_full History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene
title_fullStr History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene
title_full_unstemmed History of the Giraffe Pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the Arctic Circle during the warm Eocene
title_sort history of the giraffe pipe locality inferred from microfossil remains: a thriving freshwater ecosystem near the arctic circle during the warm eocene
publisher The Paleontological Society
publishDate 2023
url https://doi.org/10.1017/jpa.2022.101
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geographic Arctic
Canada
Northwest Territories
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Canada
Northwest Territories
genre Arctic
Climate change
Northwest Territories
genre_facet Arctic
Climate change
Northwest Territories
op_source https://doi.org/10.1017/jpa.2022.101
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container_title Journal of Paleontology
container_volume 97
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container_start_page 271
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