Response of Mangroves to Late Holocene Sea-Level Change: Palaeoecological Evidence from Sumatra, Indonesia
This study was conducted with aim to reconstruct the late Holocene mangrove history and to investigate if mangroves can be resilient to current and projected sea-level rise (SLR). The palynological record from a sediment core in the Mendahara Ilir region (MI) in Sumatra was compared with available s...
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| Veröffentlicht in: | Wetlands (Wilmington, N.C.) N.C.), 2019-10, Vol.39 (5), p.1103-1118 |
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| creator | Setyaningsih, Christina Ani Biagioni, Siria Saad, Asmadi Kashima, Kaoru Sabiham, Supiandi Behling, Hermann |
| description | This study was conducted with aim to reconstruct the late Holocene mangrove history and to investigate if mangroves can be resilient to current and projected sea-level rise (SLR). The palynological record from a sediment core in the Mendahara Ilir region (MI) in Sumatra was compared with available sea level reconstructions from sites close to MI (Malacca Strait and Singapore). The palynological results show that the mangrove swamp forest was already present in MI ca. 2300 years ago. At time, the sea-level was estimated to be ca. 2 m higher than the present level, thus indicating persistence of mangroves in MI for the current global increase scenario of more than 1 m SLR by 2100. However, the estimated rate of change from the MI core are ca. 2.2 mm/yr. These values are much lower than current (5.0 mm/yr) and future (7 mm/yr) estimates. Thus posing a threat on the resilience and the capacity to adapt of the mangrove swamp forest. Additionally, the palynological results indicate that the mangrove swamp forests were quickly moving seaward and landward following regression and transgression phases in MI. Without a clear inland free path, such migration will be impeded under current and future projections of SLR. |
| doi_str_mv | 10.1007/s13157-019-01142-1 |
| format | Article |
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The palynological record from a sediment core in the Mendahara Ilir region (MI) in Sumatra was compared with available sea level reconstructions from sites close to MI (Malacca Strait and Singapore). The palynological results show that the mangrove swamp forest was already present in MI ca. 2300 years ago. At time, the sea-level was estimated to be ca. 2 m higher than the present level, thus indicating persistence of mangroves in MI for the current global increase scenario of more than 1 m SLR by 2100. However, the estimated rate of change from the MI core are ca. 2.2 mm/yr. These values are much lower than current (5.0 mm/yr) and future (7 mm/yr) estimates. Thus posing a threat on the resilience and the capacity to adapt of the mangrove swamp forest. Additionally, the palynological results indicate that the mangrove swamp forests were quickly moving seaward and landward following regression and transgression phases in MI. Without a clear inland free path, such migration will be impeded under current and future projections of SLR.</description><identifier>ISSN: 0277-5212</identifier><identifier>EISSN: 1943-6246</identifier><identifier>DOI: 10.1007/s13157-019-01142-1</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Aquaculture ; Biodiversity ; Biomedical and Life Sciences ; Climate change ; Coastal Sciences ; Coasts ; Ecology ; Ecosystems ; Environmental Management ; Floods ; Flowers & plants ; Forests ; Freshwater & Marine Ecology ; Holocene ; Hydrogeology ; Landscape Ecology ; Life Sciences ; Mangrove swamps ; Mangroves ; Palynology ; Photosynthesis ; Rain ; Resilience ; River ecology ; Sea level ; Sedimentation & deposition ; Sediments ; Soil erosion ; Vegetation ; Wetlands and Climate Change</subject><ispartof>Wetlands (Wilmington, N.C.), 2019-10, Vol.39 (5), p.1103-1118</ispartof><rights>Society of Wetland Scientists 2019</rights><rights>Society of Wetland Scientists 2019.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c385t-517e52d466768c8be51628da977084a9a9a904f7d855010dfa4df973b652a46e3</citedby><cites>FETCH-LOGICAL-c385t-517e52d466768c8be51628da977084a9a9a904f7d855010dfa4df973b652a46e3</cites><orcidid>0000-0001-9195-7809</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13157-019-01142-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2919541624?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,21367,27901,27902,33721,41464,42533,43781,51294</link.rule.ids></links><search><creatorcontrib>Setyaningsih, Christina Ani</creatorcontrib><creatorcontrib>Biagioni, Siria</creatorcontrib><creatorcontrib>Saad, Asmadi</creatorcontrib><creatorcontrib>Kashima, Kaoru</creatorcontrib><creatorcontrib>Sabiham, Supiandi</creatorcontrib><creatorcontrib>Behling, Hermann</creatorcontrib><title>Response of Mangroves to Late Holocene Sea-Level Change: Palaeoecological Evidence from Sumatra, Indonesia</title><title>Wetlands (Wilmington, N.C.)</title><addtitle>Wetlands</addtitle><description>This study was conducted with aim to reconstruct the late Holocene mangrove history and to investigate if mangroves can be resilient to current and projected sea-level rise (SLR). 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Without a clear inland free path, such migration will be impeded under current and future projections of SLR.</description><subject>Aquaculture</subject><subject>Biodiversity</subject><subject>Biomedical and Life Sciences</subject><subject>Climate change</subject><subject>Coastal Sciences</subject><subject>Coasts</subject><subject>Ecology</subject><subject>Ecosystems</subject><subject>Environmental Management</subject><subject>Floods</subject><subject>Flowers & plants</subject><subject>Forests</subject><subject>Freshwater & Marine Ecology</subject><subject>Holocene</subject><subject>Hydrogeology</subject><subject>Landscape Ecology</subject><subject>Life Sciences</subject><subject>Mangrove swamps</subject><subject>Mangroves</subject><subject>Palynology</subject><subject>Photosynthesis</subject><subject>Rain</subject><subject>Resilience</subject><subject>River ecology</subject><subject>Sea level</subject><subject>Sedimentation & deposition</subject><subject>Sediments</subject><subject>Soil erosion</subject><subject>Vegetation</subject><subject>Wetlands and Climate Change</subject><issn>0277-5212</issn><issn>1943-6246</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kNFKwzAUhoMoOKcv4FXAW6M5adK03smYblBRnF6HrD2dHV0zk27g25tZwTsJh9x8_38OHyGXwG-Ac30bIAGlGYc8DkjB4IiMIJcJS4VMj8mIC62ZEiBOyVkIa84hFQJGZP2KYeu6gNTV9Ml2K-_2GGjvaGF7pDPXuhI7pAu0rMA9tnTyESm8oy-2teiwjMSqKW1Lp_umwq5EWnu3oYvdxvbeXtN5V7kOQ2PPyUlt24AXv_-YvD9M3yYzVjw_zif3BSuTTPVMgUYlKpmmOs3KbIkqnppVNteaZ9Lmh8dlratMKQ68qq2s6lwny1QJK1NMxuRq6N1697nD0Ju12_kurjQih1zJ2CcjJQaq9C4Ej7XZ-mZj_ZcBbg5OzeDURKfmx6mBGEqGUIhwtOD_qv9JfQN1H3jP</recordid><startdate>20191001</startdate><enddate>20191001</enddate><creator>Setyaningsih, Christina Ani</creator><creator>Biagioni, Siria</creator><creator>Saad, Asmadi</creator><creator>Kashima, Kaoru</creator><creator>Sabiham, Supiandi</creator><creator>Behling, Hermann</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><orcidid>https://orcid.org/0000-0001-9195-7809</orcidid></search><sort><creationdate>20191001</creationdate><title>Response of Mangroves to Late Holocene Sea-Level Change: Palaeoecological Evidence from Sumatra, Indonesia</title><author>Setyaningsih, Christina Ani ; Biagioni, Siria ; Saad, Asmadi ; Kashima, Kaoru ; Sabiham, Supiandi ; Behling, Hermann</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c385t-517e52d466768c8be51628da977084a9a9a904f7d855010dfa4df973b652a46e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Aquaculture</topic><topic>Biodiversity</topic><topic>Biomedical and Life Sciences</topic><topic>Climate change</topic><topic>Coastal Sciences</topic><topic>Coasts</topic><topic>Ecology</topic><topic>Ecosystems</topic><topic>Environmental Management</topic><topic>Floods</topic><topic>Flowers & plants</topic><topic>Forests</topic><topic>Freshwater & Marine Ecology</topic><topic>Holocene</topic><topic>Hydrogeology</topic><topic>Landscape Ecology</topic><topic>Life Sciences</topic><topic>Mangrove swamps</topic><topic>Mangroves</topic><topic>Palynology</topic><topic>Photosynthesis</topic><topic>Rain</topic><topic>Resilience</topic><topic>River ecology</topic><topic>Sea level</topic><topic>Sedimentation & deposition</topic><topic>Sediments</topic><topic>Soil erosion</topic><topic>Vegetation</topic><topic>Wetlands and Climate Change</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Setyaningsih, Christina Ani</creatorcontrib><creatorcontrib>Biagioni, Siria</creatorcontrib><creatorcontrib>Saad, Asmadi</creatorcontrib><creatorcontrib>Kashima, Kaoru</creatorcontrib><creatorcontrib>Sabiham, Supiandi</creatorcontrib><creatorcontrib>Behling, Hermann</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Environmental Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><jtitle>Wetlands (Wilmington, N.C.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Setyaningsih, Christina Ani</au><au>Biagioni, Siria</au><au>Saad, Asmadi</au><au>Kashima, Kaoru</au><au>Sabiham, Supiandi</au><au>Behling, Hermann</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Response of Mangroves to Late Holocene Sea-Level Change: Palaeoecological Evidence from Sumatra, Indonesia</atitle><jtitle>Wetlands (Wilmington, N.C.)</jtitle><stitle>Wetlands</stitle><date>2019-10-01</date><risdate>2019</risdate><volume>39</volume><issue>5</issue><spage>1103</spage><epage>1118</epage><pages>1103-1118</pages><issn>0277-5212</issn><eissn>1943-6246</eissn><abstract>This study was conducted with aim to reconstruct the late Holocene mangrove history and to investigate if mangroves can be resilient to current and projected sea-level rise (SLR). The palynological record from a sediment core in the Mendahara Ilir region (MI) in Sumatra was compared with available sea level reconstructions from sites close to MI (Malacca Strait and Singapore). The palynological results show that the mangrove swamp forest was already present in MI ca. 2300 years ago. At time, the sea-level was estimated to be ca. 2 m higher than the present level, thus indicating persistence of mangroves in MI for the current global increase scenario of more than 1 m SLR by 2100. However, the estimated rate of change from the MI core are ca. 2.2 mm/yr. These values are much lower than current (5.0 mm/yr) and future (7 mm/yr) estimates. Thus posing a threat on the resilience and the capacity to adapt of the mangrove swamp forest. Additionally, the palynological results indicate that the mangrove swamp forests were quickly moving seaward and landward following regression and transgression phases in MI. Without a clear inland free path, such migration will be impeded under current and future projections of SLR.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s13157-019-01142-1</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0001-9195-7809</orcidid></addata></record> |
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| subjects | Aquaculture Biodiversity Biomedical and Life Sciences Climate change Coastal Sciences Coasts Ecology Ecosystems Environmental Management Floods Flowers & plants Forests Freshwater & Marine Ecology Holocene Hydrogeology Landscape Ecology Life Sciences Mangrove swamps Mangroves Palynology Photosynthesis Rain Resilience River ecology Sea level Sedimentation & deposition Sediments Soil erosion Vegetation Wetlands and Climate Change |
| title | Response of Mangroves to Late Holocene Sea-Level Change: Palaeoecological Evidence from Sumatra, Indonesia |
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