Patterns and drivers of development in a west Amazonian peatland during the late Holocene

Amazonian peatlands sequester and store large amounts of carbon below ground and contribute to regional biodiversity. They also present an outstanding opportunity for palaeoecological research. This study uses multiple peat cores to improve our understanding of the long-term development of a peatland (Quistococha) in Peruvian Amazonia, by providing a reconstruction of the spatial patterns of vegetation change and peat accumulation over time across the site. Peat cores taken along transects totalling c. 5 km were used to establish the peat thickness and visible stratigraphy. Of 29 new peat cores, four were selected for pollen analysis, supported by 15 radiocarbon dates. These complement two existing published pollen records from the site, from a peat core and a lake sediment core. Our study shows that peat initiation occurred across the site in the form of primary mire formation between 2400 and 1900 cal yr BP. Following peat initiation, five broadly similar phases of vegetation development are recorded in all the pollen sequences: Amazon floodplain, herbaceous sedge fen, mixed angiosperm flooded forest, mixed palm swamp, Mauritia-dominated palm swamp. In detail, there are differences in the pattern and timing of vegetation change between the sequences. Much of this spatial variation is likely to be the result of the underlying substrate topography. In addition, we find that the difference in vegetation composition between core sites was greater during the early stages of peat accumulation at Quistococha than it is today. Such spatial and temporal variability has significant implications for computer modelling of carbon accumulation in tropical peatlands and, consequently, our understanding of their role in the global carbon cycle. Our findings highlight key challenges for numerical modelling on Holocene timescales, namely the difficulty in quantifying long-term variations in primary productivity, the variable influence of sediment input on carbon accumulation during the early stages of peatland formation, and the difficulty of modelling water tables in sites with variable underlying topography.

Saved in:
Bibliographic Details
Main Authors: Kelly, Thomas J., Lawson, Ian T., Roucoux, Katherine H., Baker, Timothy R., Honorio Coronado, Eurídice
Format: info:eu-repo/semantics/article biblioteca
Language:eng
Published: Elsevier 2020-02
Subjects:Paleobotánica, Turberas, Secuestro de carbono, Palinología, Mauritia flexuosa, Amazonía, Suelo turboso,
Online Access:https://hdl.handle.net/20.500.12921/436
https://doi.org/10.1016/j.quascirev.2020.106168
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-iiap-pe-20.500.12921-436
record_format koha
spelling dig-iiap-pe-20.500.12921-4362022-12-30T00:05:11Z Patterns and drivers of development in a west Amazonian peatland during the late Holocene Kelly, Thomas J. Lawson, Ian T. Roucoux, Katherine H. Baker, Timothy R. Honorio Coronado, Eurídice Paleobotánica Turberas Secuestro de carbono Palinología Mauritia flexuosa Amazonía Suelo turboso Amazonian peatlands sequester and store large amounts of carbon below ground and contribute to regional biodiversity. They also present an outstanding opportunity for palaeoecological research. This study uses multiple peat cores to improve our understanding of the long-term development of a peatland (Quistococha) in Peruvian Amazonia, by providing a reconstruction of the spatial patterns of vegetation change and peat accumulation over time across the site. Peat cores taken along transects totalling c. 5 km were used to establish the peat thickness and visible stratigraphy. Of 29 new peat cores, four were selected for pollen analysis, supported by 15 radiocarbon dates. These complement two existing published pollen records from the site, from a peat core and a lake sediment core. Our study shows that peat initiation occurred across the site in the form of primary mire formation between 2400 and 1900 cal yr BP. Following peat initiation, five broadly similar phases of vegetation development are recorded in all the pollen sequences: Amazon floodplain, herbaceous sedge fen, mixed angiosperm flooded forest, mixed palm swamp, Mauritia-dominated palm swamp. In detail, there are differences in the pattern and timing of vegetation change between the sequences. Much of this spatial variation is likely to be the result of the underlying substrate topography. In addition, we find that the difference in vegetation composition between core sites was greater during the early stages of peat accumulation at Quistococha than it is today. Such spatial and temporal variability has significant implications for computer modelling of carbon accumulation in tropical peatlands and, consequently, our understanding of their role in the global carbon cycle. Our findings highlight key challenges for numerical modelling on Holocene timescales, namely the difficulty in quantifying long-term variations in primary productivity, the variable influence of sediment input on carbon accumulation during the early stages of peatland formation, and the difficulty of modelling water tables in sites with variable underlying topography. Royal Geographical Society, NERC (grant ref. NE/H011773/1) Revisión por pares. 2020-03-04T16:58:25Z 2020-03-04T16:58:25Z 2020-02 info:eu-repo/semantics/article Quaternary Science Reviews, 230: 106168 0277-3791 https://hdl.handle.net/20.500.12921/436 Quaternary Science Reviews https://doi.org/10.1016/j.quascirev.2020.106168 eng info:eu-repo/semantics/article https://www.sciencedirect.com/science/article/abs/pii/S0277379119309588 info:eu-repo/semantics/closedAccess Copyright © 2020 Elsevier application/pdf application/pdf text/plain; charset=utf-8 Elsevier Instituto de Investigaciones de la Amazonía Peruana Repositorio Institucional - IIAP
institution IIAP PE
collection DSpace
country Perú
countrycode PE
component Bibliográfico
access En linea
databasecode dig-iiap-pe
tag biblioteca
region America del Sur
libraryname Biblioteca del IIAP Perú
language eng
topic Paleobotánica
Turberas
Secuestro de carbono
Palinología
Mauritia flexuosa
Amazonía
Suelo turboso
Paleobotánica
Turberas
Secuestro de carbono
Palinología
Mauritia flexuosa
Amazonía
Suelo turboso
spellingShingle Paleobotánica
Turberas
Secuestro de carbono
Palinología
Mauritia flexuosa
Amazonía
Suelo turboso
Paleobotánica
Turberas
Secuestro de carbono
Palinología
Mauritia flexuosa
Amazonía
Suelo turboso
Kelly, Thomas J.
Lawson, Ian T.
Roucoux, Katherine H.
Baker, Timothy R.
Honorio Coronado, Eurídice
Patterns and drivers of development in a west Amazonian peatland during the late Holocene
description Amazonian peatlands sequester and store large amounts of carbon below ground and contribute to regional biodiversity. They also present an outstanding opportunity for palaeoecological research. This study uses multiple peat cores to improve our understanding of the long-term development of a peatland (Quistococha) in Peruvian Amazonia, by providing a reconstruction of the spatial patterns of vegetation change and peat accumulation over time across the site. Peat cores taken along transects totalling c. 5 km were used to establish the peat thickness and visible stratigraphy. Of 29 new peat cores, four were selected for pollen analysis, supported by 15 radiocarbon dates. These complement two existing published pollen records from the site, from a peat core and a lake sediment core. Our study shows that peat initiation occurred across the site in the form of primary mire formation between 2400 and 1900 cal yr BP. Following peat initiation, five broadly similar phases of vegetation development are recorded in all the pollen sequences: Amazon floodplain, herbaceous sedge fen, mixed angiosperm flooded forest, mixed palm swamp, Mauritia-dominated palm swamp. In detail, there are differences in the pattern and timing of vegetation change between the sequences. Much of this spatial variation is likely to be the result of the underlying substrate topography. In addition, we find that the difference in vegetation composition between core sites was greater during the early stages of peat accumulation at Quistococha than it is today. Such spatial and temporal variability has significant implications for computer modelling of carbon accumulation in tropical peatlands and, consequently, our understanding of their role in the global carbon cycle. Our findings highlight key challenges for numerical modelling on Holocene timescales, namely the difficulty in quantifying long-term variations in primary productivity, the variable influence of sediment input on carbon accumulation during the early stages of peatland formation, and the difficulty of modelling water tables in sites with variable underlying topography.
format info:eu-repo/semantics/article
topic_facet Paleobotánica
Turberas
Secuestro de carbono
Palinología
Mauritia flexuosa
Amazonía
Suelo turboso
author Kelly, Thomas J.
Lawson, Ian T.
Roucoux, Katherine H.
Baker, Timothy R.
Honorio Coronado, Eurídice
author_facet Kelly, Thomas J.
Lawson, Ian T.
Roucoux, Katherine H.
Baker, Timothy R.
Honorio Coronado, Eurídice
author_sort Kelly, Thomas J.
title Patterns and drivers of development in a west Amazonian peatland during the late Holocene
title_short Patterns and drivers of development in a west Amazonian peatland during the late Holocene
title_full Patterns and drivers of development in a west Amazonian peatland during the late Holocene
title_fullStr Patterns and drivers of development in a west Amazonian peatland during the late Holocene
title_full_unstemmed Patterns and drivers of development in a west Amazonian peatland during the late Holocene
title_sort patterns and drivers of development in a west amazonian peatland during the late holocene
publisher Elsevier
publishDate 2020-02
url https://hdl.handle.net/20.500.12921/436
https://doi.org/10.1016/j.quascirev.2020.106168
work_keys_str_mv AT kellythomasj patternsanddriversofdevelopmentinawestamazonianpeatlandduringthelateholocene
AT lawsoniant patternsanddriversofdevelopmentinawestamazonianpeatlandduringthelateholocene
AT roucouxkatherineh patternsanddriversofdevelopmentinawestamazonianpeatlandduringthelateholocene
AT bakertimothyr patternsanddriversofdevelopmentinawestamazonianpeatlandduringthelateholocene
AT honoriocoronadoeuridice patternsanddriversofdevelopmentinawestamazonianpeatlandduringthelateholocene
_version_ 1756091455847268352