Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida
Sea level rise and the associated inland shift of the marsh-mangrove ecotone in south Florida have raised many scientific and management concerns in recent years. Holocene paleoecological records can provide an important baseline to shed light on the long-term dynamics of vegetation changes across t...
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ftzenodo:oai:zenodo.org:5006823 2024-09-15T18:24:23+00:00 Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida Yao, Qiang Liu, Kam-biu 2018-03-01 https://doi.org/10.5061/dryad.1j741 unknown Zenodo https://doi.org/10.1371/journal.pone.0173670 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.1j741 oai:zenodo.org:5006823 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode BACON LOI info:eu-repo/semantics/other 2018 ftzenodo https://doi.org/10.5061/dryad.1j74110.1371/journal.pone.0173670 2024-07-26T10:30:02Z Sea level rise and the associated inland shift of the marsh-mangrove ecotone in south Florida have raised many scientific and management concerns in recent years. Holocene paleoecological records can provide an important baseline to shed light on the long-term dynamics of vegetation changes across this ecotone in the past, which is needed to predict the future. In this study, we present palynological, X-ray fluorescence, and loss-on ignition data from four sedimentary cores recovered from a 20-km marine-to-freshwater transect along the Shark River Estuary, southwest Everglades, to document the patterns and processes of coastal vegetation changes in response to sea level rise since the mid-Holocene. Our record indicates that freshwater marsh progressively replaced marl prairies at the Shark River Estuary between 5700 and 4400 cal yr BP. As marine transgression continued, marine influence reached the threshold necessary for mangroves to establish at the current mouth of the Shark River Slough at 3800 cal yr BP. During the next 3000 years, although sea level rise in the Western North Atlantic slowed down to 0.4 mm/yr, a spatial and temporal gradient was evident as the marsh-mangrove ecotone shifted inland by 20 km from 3800 to 800 cal yr BP, accompanied by a gradual landward replacement of freshwater marsh by mangrove forest. If sea level continues to rise at 2.33 mm/yr in the 21st century in south Florida, it is possible that marine influence will reach the threshold for mangroves to establish in the central Everglades, and we could expect a much more aggressive mangrove encroachment toward the northern and interior parts of south Florida in the next few centuries. LOI data Loss-on-ignition data for core SRS-4, SRS-5, SRS-6, and SRM Pollen data Pollen data for core SRS-4, SRS-5, SRS-6, and SRM XRF data X-ray fluorescence data for core SRS-4, SRS-5, SRS-6, and SRM SRM BACON settings and ages BACON data for core SRM Other/Unknown Material North Atlantic Zenodo |
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BACON LOI Yao, Qiang Liu, Kam-biu Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida |
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BACON LOI |
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Sea level rise and the associated inland shift of the marsh-mangrove ecotone in south Florida have raised many scientific and management concerns in recent years. Holocene paleoecological records can provide an important baseline to shed light on the long-term dynamics of vegetation changes across this ecotone in the past, which is needed to predict the future. In this study, we present palynological, X-ray fluorescence, and loss-on ignition data from four sedimentary cores recovered from a 20-km marine-to-freshwater transect along the Shark River Estuary, southwest Everglades, to document the patterns and processes of coastal vegetation changes in response to sea level rise since the mid-Holocene. Our record indicates that freshwater marsh progressively replaced marl prairies at the Shark River Estuary between 5700 and 4400 cal yr BP. As marine transgression continued, marine influence reached the threshold necessary for mangroves to establish at the current mouth of the Shark River Slough at 3800 cal yr BP. During the next 3000 years, although sea level rise in the Western North Atlantic slowed down to 0.4 mm/yr, a spatial and temporal gradient was evident as the marsh-mangrove ecotone shifted inland by 20 km from 3800 to 800 cal yr BP, accompanied by a gradual landward replacement of freshwater marsh by mangrove forest. If sea level continues to rise at 2.33 mm/yr in the 21st century in south Florida, it is possible that marine influence will reach the threshold for mangroves to establish in the central Everglades, and we could expect a much more aggressive mangrove encroachment toward the northern and interior parts of south Florida in the next few centuries. LOI data Loss-on-ignition data for core SRS-4, SRS-5, SRS-6, and SRM Pollen data Pollen data for core SRS-4, SRS-5, SRS-6, and SRM XRF data X-ray fluorescence data for core SRS-4, SRS-5, SRS-6, and SRM SRM BACON settings and ages BACON data for core SRM |
format |
Other/Unknown Material |
author |
Yao, Qiang Liu, Kam-biu |
author_facet |
Yao, Qiang Liu, Kam-biu |
author_sort |
Yao, Qiang |
title |
Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida |
title_short |
Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida |
title_full |
Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida |
title_fullStr |
Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida |
title_full_unstemmed |
Data from: Dynamics of marsh-mangrove ecotone since the mid-Holocene: a palynological study of mangrove encroachment and sea level rise in the Shark River Estuary, Florida |
title_sort |
data from: dynamics of marsh-mangrove ecotone since the mid-holocene: a palynological study of mangrove encroachment and sea level rise in the shark river estuary, florida |
publisher |
Zenodo |
publishDate |
2018 |
url |
https://doi.org/10.5061/dryad.1j741 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://doi.org/10.1371/journal.pone.0173670 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.1j741 oai:zenodo.org:5006823 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode |
op_doi |
https://doi.org/10.5061/dryad.1j74110.1371/journal.pone.0173670 |
_version_ |
1810464728846172160 |