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On October 22, 2024, 4:52:21 PM UTC,
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Updated description of Algal-Induced Biogeomorphic Feedbacks Lay the Groundwork for Coastal Wetland Development from
Ecosystem establishment under adverse geophysical conditions is often studied within the framework of windows of opportunity, which predicts ecosystems to establish when geophysical disturbances are temporarily reduced. However, the role of biogeophysical interactions in this framework is less well understood. The establishment of saltmarsh vegetation on tidal flats, for example, is limited by abiotic factors such as hydrodynamics, sediment stability and drainage. On tidal flats, we observe high densities of plant seedlings on raised sediment ridges colonized by algal mats (Vaucheria sp.). Such ridges were previously found to have higher sediment strength than substrate without algae. Here, we investigate whether these measurements can be explained by geophysical factors only, or that biological (Vaucheria-induced) processes influence tidal marsh establishment by forming stabilized bedforms. We perform two experiments under controlled mesocosm conditions, to test the hypotheses that i) Vaucheria grows better on elevated topographic relief, ii) the binding force of their algal filaments increases sediment strength, which consequently iii) creates elevated topographic relief that further facilitates algal growth. Our experimental results confirm the existence of this algal-induced biogeomorphic feedback cycle. These findings reveal that primitive organisms like Vaucheria may contribute significantly to tidal marsh formation by creating elevated and stabilized substrate. We thus show that biogeophysical feedbacks can “widen” the windows of opportunity for further ecosystem establishment. Our results could be useful for the design of managed realignment projects aimed at restoring the unique ecosystem services of coastal wetlands, such as habitat biodiversity, carbon sequestration potential and nature-based flood defense.
toEcosystem establishment under adverse geophysical conditions is often studied within the “windows of opportunity” framework, identifying disturbance-free periods (e.g., calm wave climate) where species can overcome establishment thresholds. However, the role of biogeophysical interactions in this framework is less well understood. The establishment of saltmarsh vegetation on tidal flats, for example, is limited by abiotic factors such as hydrodynamics, sediment stability and drainage. On tidal flats, raised sediment ridges colonized by algal mats (Vaucheria sp.) appear to accomodate high densities of plant seedlings. Such ridges were previously found to have higher sediment strength than substratum without algae. Here, we investigate whether these measurements can be explained by geophysical factors only, or that biological (Vaucheria-induced) processes influence tidal marsh establishment by forming stabilized bedforms. We performed two experiments under controlled mesocosm conditions, to test the hypotheses that i) Vaucheria grows better on elevated topographic relief, that ii) the binding force of their algal filaments increases sediment strength, and that iii) Vaucheria consequently creates elevated topographic relief that further facilitates algal growth. Our experimental results confirm the existence of this algal-induced biogeomorphic feedback cycle. These findings imply that benthic algae like Vaucheria may contribute significantly to tidal marsh formation by creating elevated and stabilized substratum. This suggests biogeophysical feedbacks can “widen” the windows of opportunity for further ecosystem establishment. Our results could be useful for the design of managed realignment projects aimed at restoring the unique ecosystem services of coastal wetlands, such as habitat biodiversity, carbon sequestration potential and nature-based flood defense.
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Changed the version of Algal-Induced Biogeomorphic Feedbacks Lay the Groundwork for Coastal Wetland Development to 4 (previously 3)
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| 7 | "creators": "[{\"firstname\":\"Roeland C.\",\"lastname\":\"van de | 7 | "creators": "[{\"firstname\":\"Roeland C.\",\"lastname\":\"van de | ||
| 8 | Vijsel\",\"affiliation\":\"Royal Netherlands Institute for Sea | 8 | Vijsel\",\"affiliation\":\"Royal Netherlands Institute for Sea | ||
| 9 | scorrespondingauthor\":true},{\"firstname\":\"Jim\",\"lastname\":\"van | 9 | scorrespondingauthor\":true},{\"firstname\":\"Jim\",\"lastname\":\"van | ||
| 10 | Belzen\",\"affiliation\":\"Royal Netherlands Institute for Sea | 10 | Belzen\",\"affiliation\":\"Royal Netherlands Institute for Sea | ||
| 11 | ddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Tjeerd | 11 | ddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Tjeerd | ||
| 12 | J.\",\"lastname\":\"Bouma\",\"affiliation\":\"Royal Netherlands | 12 | J.\",\"lastname\":\"Bouma\",\"affiliation\":\"Royal Netherlands | ||
| 13 | Institute for Sea | 13 | Institute for Sea | ||
| 14 | respondingauthor\":false},{\"firstname\":\"Daphne\",\"lastname\":\"van | 14 | respondingauthor\":false},{\"firstname\":\"Daphne\",\"lastname\":\"van | ||
| 15 | der Wal\",\"affiliation\":\"Royal Netherlands Institute for Sea | 15 | der Wal\",\"affiliation\":\"Royal Netherlands Institute for Sea | ||
| 16 | rrespondingauthor\":false},{\"firstname\":\"Johan\",\"lastname\":\"van | 16 | rrespondingauthor\":false},{\"firstname\":\"Johan\",\"lastname\":\"van | ||
| 17 | de Koppel\",\"affiliation\":\"Royal Netherlands Institute for Sea | 17 | de Koppel\",\"affiliation\":\"Royal Netherlands Institute for Sea | ||
| 18 | 275\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | 18 | 275\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | ||
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| 21 | 021-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"The | 21 | 021-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"The | ||
| 22 | entire dataset used to make all figures and do all calculations in the | 22 | entire dataset used to make all figures and do all calculations in the | ||
| 23 | manuscript \\\"van de Vijsel et al. (Submitted). Algal-induced | 23 | manuscript \\\"van de Vijsel et al. (Submitted). Algal-induced | ||
| 24 | biogeomorphic feedbacks lay the groundwork for coastal wetland | 24 | biogeomorphic feedbacks lay the groundwork for coastal wetland | ||
| 25 | development\\\". Final complete, finetuned version | 25 | development\\\". Final complete, finetuned version | ||
| 26 | 021-09-28T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Added | 26 | 021-09-28T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Added | ||
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| 28 | 2021-10-10T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Made | 28 | 2021-10-10T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Made | ||
| 29 | dataset publicly available after manuscript was accepted for | 29 | dataset publicly available after manuscript was accepted for | ||
| 30 | publication in JGR | 30 | publication in JGR | ||
| 31 | 021-10-13T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Added | 31 | 021-10-13T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Added | ||
| 32 | the DOI of the article published in JGR Biogeosciences.\"}]", | 32 | the DOI of the article published in JGR Biogeosciences.\"}]", | ||
| 33 | "deposit_date": "2021-03-23", | 33 | "deposit_date": "2021-03-23", | ||
| 34 | "depositor": "Roeland van de Vijsel", | 34 | "depositor": "Roeland van de Vijsel", | ||
| 35 | "distribution_date": "2021-03-23", | 35 | "distribution_date": "2021-03-23", | ||
| 36 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 36 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 37 | Institute for Sea Research)", | 37 | Institute for Sea Research)", | ||
| 38 | "doi_date_published": "2021-10-11", | 38 | "doi_date_published": "2021-10-11", | ||
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| 44 | modelling HPP\"}]", | 44 | modelling HPP\"}]", | ||
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| 54 | "notes": "Ecosystem establishment under adverse geophysical | 54 | "notes": "Ecosystem establishment under adverse geophysical | ||
| n | 55 | conditions is often studied within the framework of windows of | n | 55 | conditions is often studied within the \u201cwindows of |
| 56 | opportunity, which predicts ecosystems to establish when geophysical | 56 | opportunity\u201d framework, identifying disturbance-free periods | ||
| 57 | disturbances are temporarily reduced. However, the role of | 57 | (e.g., calm wave climate) where species can overcome establishment | ||
| 58 | biogeophysical interactions in this framework is less well understood. | 58 | thresholds. However, the role of biogeophysical interactions in this | ||
| 59 | The establishment of saltmarsh vegetation on tidal flats, for example, | 59 | framework is less well understood. The establishment of saltmarsh | ||
| 60 | is limited by abiotic factors such as hydrodynamics, sediment | 60 | vegetation on tidal flats, for example, is limited by abiotic factors | ||
| 61 | stability and drainage. On tidal flats, we observe high densities of | 61 | such as hydrodynamics, sediment stability and drainage. On tidal | ||
| 62 | plant seedlings on raised sediment ridges colonized by algal mats | 62 | flats, raised sediment ridges colonized by algal mats (Vaucheria sp.) | ||
| 63 | (Vaucheria sp.). Such ridges were previously found to have higher | 63 | appear to accomodate high densities of plant seedlings. Such ridges | ||
| 64 | sediment strength than substrate without algae. Here, we investigate | 64 | were previously found to have higher sediment strength than substratum | ||
| 65 | whether these measurements can be explained by geophysical factors | 65 | without algae. Here, we investigate whether these measurements can be | ||
| 66 | only, or that biological (Vaucheria-induced) processes influence tidal | 66 | explained by geophysical factors only, or that biological | ||
| 67 | marsh establishment by forming stabilized bedforms. We perform two | 67 | (Vaucheria-induced) processes influence tidal marsh establishment by | ||
| 68 | experiments under controlled mesocosm conditions, to test the | 68 | forming stabilized bedforms. We performed two experiments under | ||
| 69 | hypotheses that i) Vaucheria grows better on elevated topographic | 69 | controlled mesocosm conditions, to test the hypotheses that i) | ||
| 70 | relief, ii) the binding force of their algal filaments increases | 70 | Vaucheria grows better on elevated topographic relief, that ii) the | ||
| 71 | sediment strength, which consequently iii) creates elevated | 71 | binding force of their algal filaments increases sediment strength, | ||
| 72 | and that iii) Vaucheria consequently creates elevated topographic | ||||
| 72 | topographic relief that further facilitates algal growth. Our | 73 | relief that further facilitates algal growth. Our experimental results | ||
| 73 | experimental results confirm the existence of this algal-induced | 74 | confirm the existence of this algal-induced biogeomorphic feedback | ||
| 74 | biogeomorphic feedback cycle. These findings reveal that primitive | 75 | cycle. These findings imply that benthic algae like Vaucheria may | ||
| 75 | organisms like Vaucheria may contribute significantly to tidal marsh | 76 | contribute significantly to tidal marsh formation by creating elevated | ||
| 76 | formation by creating elevated and stabilized substrate. We thus show | 77 | and stabilized substratum. This suggests biogeophysical feedbacks can | ||
| 77 | that biogeophysical feedbacks can \u201cwiden\u201d the windows of | 78 | \u201cwiden\u201d the windows of opportunity for further ecosystem | ||
| 78 | opportunity for further ecosystem establishment. Our results could be | 79 | establishment. Our results could be useful for the design of managed | ||
| 79 | useful for the design of managed realignment projects aimed at | 80 | realignment projects aimed at restoring the unique ecosystem services | ||
| 80 | restoring the unique ecosystem services of coastal wetlands, such as | 81 | of coastal wetlands, such as habitat biodiversity, carbon | ||
| 81 | habitat biodiversity, carbon sequestration potential and nature-based | 82 | sequestration potential and nature-based flood defense.", | ||
| 82 | flood defense.", | ||||
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| 264 | "display_name": "Coastal wetlands mudflat saltmarsh | 264 | "display_name": "Coastal wetlands mudflat saltmarsh | ||
| 265 | biogeomorphology algal mats vegetation sediment strength drainag", | 265 | biogeomorphology algal mats vegetation sediment strength drainag", | ||
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| 267 | "name": "Coastal wetlands mudflat saltmarsh biogeomorphology | 267 | "name": "Coastal wetlands mudflat saltmarsh biogeomorphology | ||
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| 273 | "title": "Algal-Induced Biogeomorphic Feedbacks Lay the Groundwork | 273 | "title": "Algal-Induced Biogeomorphic Feedbacks Lay the Groundwork | ||
| 274 | for Coastal Wetland Development", | 274 | for Coastal Wetland Development", | ||
| 275 | "type": "dataset", | 275 | "type": "dataset", | ||
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