Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C

Several coastal ecosystems-most notably mangroves and tidal marshes-exhibit biogenic feedbacks that are facilitating adjustment to relative sea-level rise (RSLR), including the sequestration of carbon and the trapping of mineral sediment1. The stability of reef-top habitats under RSLR is similarly l...

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Main Authors: Saintilan, Neil, Horton, Benjamin Peter, Törnqvist, Torbjörn E., Ashe, Erica L., Khan, Nicole S., Schuerch, Mark, Perry, Chris, Kopp, Robert E., Garner, Gregory G., Murray, Nicholas, Rogers, Kerrylee, Albert, Simon, Kelleway, Jeffrey, Shaw, Timothy Adam, Woodroffe, Colin D., Lovelock, Catherine E., Goddard, Madeline M., Hutley, Lindsay B., Kovalenko, Katya, Feher, Laura, Guntenspergen, Glenn
Other Authors: Asian School of the Environment
Format: Article
Language:English
Published: 2024
Subjects:
Online Access:https://hdl.handle.net/10356/174165
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Institution: Nanyang Technological University
Language: English
id sg-ntu-dr.10356-174165
record_format dspace
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Earth and Environmental Sciences
Coastal waters
Coral reef
spellingShingle Earth and Environmental Sciences
Coastal waters
Coral reef
Saintilan, Neil
Horton, Benjamin Peter
Törnqvist, Torbjörn E.
Ashe, Erica L.
Khan, Nicole S.
Schuerch, Mark
Perry, Chris
Kopp, Robert E.
Garner, Gregory G.
Murray, Nicholas
Rogers, Kerrylee
Albert, Simon
Kelleway, Jeffrey
Shaw, Timothy Adam
Woodroffe, Colin D.
Lovelock, Catherine E.
Goddard, Madeline M.
Hutley, Lindsay B.
Kovalenko, Katya
Feher, Laura
Guntenspergen, Glenn
Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C
description Several coastal ecosystems-most notably mangroves and tidal marshes-exhibit biogenic feedbacks that are facilitating adjustment to relative sea-level rise (RSLR), including the sequestration of carbon and the trapping of mineral sediment1. The stability of reef-top habitats under RSLR is similarly linked to reef-derived sediment accumulation and the vertical accretion of protective coral reefs2. The persistence of these ecosystems under high rates of RSLR is contested3. Here we show that the probability of vertical adjustment to RSLR inferred from palaeo-stratigraphic observations aligns with contemporary in situ survey measurements. A deficit between tidal marsh and mangrove adjustment and RSLR is likely at 4 mm yr-1 and highly likely at 7 mm yr-1 of RSLR. As rates of RSLR exceed 7 mm yr-1, the probability that reef islands destabilize through increased shoreline erosion and wave over-topping increases. Increased global warming from 1.5 °C to 2.0 °C would double the area of mapped tidal marsh exposed to 4 mm yr-1 of RSLR by between 2080 and 2100. With 3 °C of warming, nearly all the world's mangrove forests and coral reef islands and almost 40% of mapped tidal marshes are estimated to be exposed to RSLR of at least 7 mm yr-1. Meeting the Paris agreement targets would minimize disruption to coastal ecosystems.
author2 Asian School of the Environment
author_facet Asian School of the Environment
Saintilan, Neil
Horton, Benjamin Peter
Törnqvist, Torbjörn E.
Ashe, Erica L.
Khan, Nicole S.
Schuerch, Mark
Perry, Chris
Kopp, Robert E.
Garner, Gregory G.
Murray, Nicholas
Rogers, Kerrylee
Albert, Simon
Kelleway, Jeffrey
Shaw, Timothy Adam
Woodroffe, Colin D.
Lovelock, Catherine E.
Goddard, Madeline M.
Hutley, Lindsay B.
Kovalenko, Katya
Feher, Laura
Guntenspergen, Glenn
format Article
author Saintilan, Neil
Horton, Benjamin Peter
Törnqvist, Torbjörn E.
Ashe, Erica L.
Khan, Nicole S.
Schuerch, Mark
Perry, Chris
Kopp, Robert E.
Garner, Gregory G.
Murray, Nicholas
Rogers, Kerrylee
Albert, Simon
Kelleway, Jeffrey
Shaw, Timothy Adam
Woodroffe, Colin D.
Lovelock, Catherine E.
Goddard, Madeline M.
Hutley, Lindsay B.
Kovalenko, Katya
Feher, Laura
Guntenspergen, Glenn
author_sort Saintilan, Neil
title Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C
title_short Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C
title_full Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C
title_fullStr Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C
title_full_unstemmed Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C
title_sort widespread retreat of coastal habitat is likely at warming levels above 1.5 °c
publishDate 2024
url https://hdl.handle.net/10356/174165
_version_ 1800916094325620736
spelling sg-ntu-dr.10356-1741652024-04-09T00:41:15Z Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C Saintilan, Neil Horton, Benjamin Peter Törnqvist, Torbjörn E. Ashe, Erica L. Khan, Nicole S. Schuerch, Mark Perry, Chris Kopp, Robert E. Garner, Gregory G. Murray, Nicholas Rogers, Kerrylee Albert, Simon Kelleway, Jeffrey Shaw, Timothy Adam Woodroffe, Colin D. Lovelock, Catherine E. Goddard, Madeline M. Hutley, Lindsay B. Kovalenko, Katya Feher, Laura Guntenspergen, Glenn Asian School of the Environment Earth Observatory of Singapore Earth and Environmental Sciences Coastal waters Coral reef Several coastal ecosystems-most notably mangroves and tidal marshes-exhibit biogenic feedbacks that are facilitating adjustment to relative sea-level rise (RSLR), including the sequestration of carbon and the trapping of mineral sediment1. The stability of reef-top habitats under RSLR is similarly linked to reef-derived sediment accumulation and the vertical accretion of protective coral reefs2. The persistence of these ecosystems under high rates of RSLR is contested3. Here we show that the probability of vertical adjustment to RSLR inferred from palaeo-stratigraphic observations aligns with contemporary in situ survey measurements. A deficit between tidal marsh and mangrove adjustment and RSLR is likely at 4 mm yr-1 and highly likely at 7 mm yr-1 of RSLR. As rates of RSLR exceed 7 mm yr-1, the probability that reef islands destabilize through increased shoreline erosion and wave over-topping increases. Increased global warming from 1.5 °C to 2.0 °C would double the area of mapped tidal marsh exposed to 4 mm yr-1 of RSLR by between 2080 and 2100. With 3 °C of warming, nearly all the world's mangrove forests and coral reef islands and almost 40% of mapped tidal marshes are estimated to be exposed to RSLR of at least 7 mm yr-1. Meeting the Paris agreement targets would minimize disruption to coastal ecosystems. Ministry of Education (MOE) National Environmental Agency (NEA) National Research Foundation (NRF) Published version We thank the authors of the IPCC projection for developing and making the sea-level rise projections available, multiple funding agencies for supporting the development of the projections, and the NASA Sea-Level Change Team for developing and hosting the IPCC AR6 Sea-Level Projection Tool. N.S. was supported by an Alexander Von Humboldt Research Award. R.E.K., G.G.G. and E.L.A. were supported by awards from the US National Aeronautics and Space Administration (80NSSC17K0698, 80NSSC20K1724 and JPL task 105393.509496.02.08.13.31) and National Science Foundation (ICER-1663807, ICER-2103754, OCE-1702587 and OCE-2002437). B. H. and T.A.S. were funded by the Ministry of Education Academic Research Fund MOE2019-T3-1-004, the National Research Foundation Singapore, and the Singapore Ministry of Education, under the Research Centres of Excellence initiative and the National Sea Level Programme Funding Initiative (Award USS-IF-2020-1), administered by the National Environment Agency, Singapore and supported by the National Research Foundation, Singapore. Any opinions, findings and conclusions or recommendations expressed in this material are those of the author(s) and do not reflect the views of the NRF, MND and NEA. T.E.T. was funded by the US National Science Foundation (OCE-0601814, EAR-1349311 and OCE-1502588). M.S. has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement no. 101037097 (REST-COAST project). C.L. was funded by the Australian Research Council award FL200100133. K.R. and C.W. were funded by the Australian Research Council Award DP210100739. The authors acknowledge PALSEA (Palaeo-Constraints on Sea-Level Rise), a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES), which in turn received support from the Swiss Academy of Sciences and the Chinese Academy of Sciences. 2024-03-18T07:08:12Z 2024-03-18T07:08:12Z 2023 Journal Article Saintilan, N., Horton, B. P., Törnqvist, T. E., Ashe, E. L., Khan, N. S., Schuerch, M., Perry, C., Kopp, R. E., Garner, G. G., Murray, N., Rogers, K., Albert, S., Kelleway, J., Shaw, T. A., Woodroffe, C. D., Lovelock, C. E., Goddard, M. M., Hutley, L. B., Kovalenko, K., ...Guntenspergen, G. (2023). Widespread retreat of coastal habitat is likely at warming levels above 1.5 °C. Nature, 621(7977), 112-119. https://dx.doi.org/10.1038/s41586-023-06448-z 0028-0836 https://hdl.handle.net/10356/174165 10.1038/s41586-023-06448-z 37648850 2-s2.0-85169160343 7977 621 112 119 en MOE2019-T3-1-004 USS-IF-2020-1 Nature © 2023 The Author(s). This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/. application/pdf