Changes
On October 22, 2024, 8:41:53 PM UTC,
-
Changed the version of Chapter 4 - Algal-induced biogeomorphic feedbacks lay the groundwork for coastal wetland development to 2 (previously 1)
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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}]", | ||
| 19 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.sc", | 19 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.sc", | ||
| 20 | "dates": | 20 | "dates": | ||
| 21 | 021-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"The | 21 | 021-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"The | ||
| 22 | dataset supporting Chapter 4 of the PhD Thesis of Roeland C. van de | 22 | dataset supporting Chapter 4 of the PhD Thesis of Roeland C. van de | ||
| 23 | Vijsel (https://doi.org/10.33612/diss.160081233).\"}]", | 23 | Vijsel (https://doi.org/10.33612/diss.160081233).\"}]", | ||
| 24 | "deposit_date": "2021-07-13", | 24 | "deposit_date": "2021-07-13", | ||
| 25 | "depositor": "Roeland van de Vijsel", | 25 | "depositor": "Roeland van de Vijsel", | ||
| 26 | "distribution_date": "2021-07-13", | 26 | "distribution_date": "2021-07-13", | ||
| 27 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 27 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 28 | Institute for Sea Research)", | 28 | Institute for Sea Research)", | ||
| 29 | "doi_date_published": "2023-11-22", | 29 | "doi_date_published": "2023-11-22", | ||
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| 31 | Scientific Research | 31 | Scientific Research | ||
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| 35 | modelling HPP\"}]", | 35 | modelling HPP\"}]", | ||
| 36 | "groups": [], | 36 | "groups": [], | ||
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| 38 | "isopen": true, | 38 | "isopen": true, | ||
| 39 | "license_id": "CC0-1.0", | 39 | "license_id": "CC0-1.0", | ||
| 40 | "license_title": "CC0 1.0", | 40 | "license_title": "CC0 1.0", | ||
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| 42 | "maintainer": null, | 42 | "maintainer": null, | ||
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| 44 | "metadata_created": "2024-10-22T11:44:14.023092", | 44 | "metadata_created": "2024-10-22T11:44:14.023092", | ||
| n | 45 | "metadata_modified": "2024-10-22T20:41:53.407542", | n | 45 | "metadata_modified": "2024-10-22T20:41:53.691403", |
| 46 | "name": "7bbsc", | 46 | "name": "7bbsc", | ||
| 47 | "notes": "Coastal wetlands provide valuable ecosystem services, | 47 | "notes": "Coastal wetlands provide valuable ecosystem services, | ||
| 48 | including biodiverse habitats, carbon sequestration potential and | 48 | including biodiverse habitats, carbon sequestration potential and | ||
| 49 | nature-based flood defense. The establishment of saltmarsh vegetation | 49 | nature-based flood defense. The establishment of saltmarsh vegetation | ||
| 50 | and other key wetland species on bare tidal flats relies on windows of | 50 | and other key wetland species on bare tidal flats relies on windows of | ||
| 51 | opportunity, which are traditionally linked to physical factors such | 51 | opportunity, which are traditionally linked to physical factors such | ||
| 52 | as hydrodynamic conditions, substrate stability and drainage. However, | 52 | as hydrodynamic conditions, substrate stability and drainage. However, | ||
| 53 | observations on tidal flats suggest that plant seedlings settle in | 53 | observations on tidal flats suggest that plant seedlings settle in | ||
| 54 | high densities on raised sedimentary ridges colonized by mats of | 54 | high densities on raised sedimentary ridges colonized by mats of | ||
| 55 | primitive filamentous algae (Vaucheria sp.). Such algal-covered ridges | 55 | primitive filamentous algae (Vaucheria sp.). Such algal-covered ridges | ||
| 56 | were previously shown to have higher sediment strength than substrate | 56 | were previously shown to have higher sediment strength than substrate | ||
| 57 | without algae. Here, we investigated whether these measurements can be | 57 | without algae. Here, we investigated whether these measurements can be | ||
| 58 | explained by physical processes only, or that biological | 58 | explained by physical processes only, or that biological | ||
| 59 | (Vaucheria-induced) processes influence early saltmarsh establishment | 59 | (Vaucheria-induced) processes influence early saltmarsh establishment | ||
| 60 | through the formation of stabilized bedforms. We performed two | 60 | through the formation of stabilized bedforms. We performed two | ||
| 61 | experiments under controlled mesocosm conditions, to test the | 61 | experiments under controlled mesocosm conditions, to test the | ||
| 62 | hypotheses that i) Vaucheria grows better on elevated topographic | 62 | hypotheses that i) Vaucheria grows better on elevated topographic | ||
| 63 | relief, ii) the binding force of their algal filaments increases | 63 | relief, ii) the binding force of their algal filaments increases | ||
| 64 | sediment strength, which consequently iii) maintains and creates | 64 | sediment strength, which consequently iii) maintains and creates | ||
| 65 | elevated topographic relief on which algal growth is further | 65 | elevated topographic relief on which algal growth is further | ||
| 66 | facilitated. The existence of this algal-induced biogeomorphic | 66 | facilitated. The existence of this algal-induced biogeomorphic | ||
| 67 | feedback cycle was confirmed in our experiments. Our findings reveal | 67 | feedback cycle was confirmed in our experiments. Our findings reveal | ||
| 68 | that halophytic plants are not the only important ecosystem engineer | 68 | that halophytic plants are not the only important ecosystem engineer | ||
| 69 | in coastal wetlands, but that fast-growing, mat- forming species like | 69 | in coastal wetlands, but that fast-growing, mat- forming species like | ||
| 70 | Vaucheria also play a major role by creating stable and elevated | 70 | Vaucheria also play a major role by creating stable and elevated | ||
| 71 | sedimentary relief. Our study indicates that biota can widen the | 71 | sedimentary relief. Our study indicates that biota can widen the | ||
| 72 | windows of opportunity for ecosystem establishment, which can be | 72 | windows of opportunity for ecosystem establishment, which can be | ||
| 73 | utilized to optimally design managed coastal realignment projects that | 73 | utilized to optimally design managed coastal realignment projects that | ||
| 74 | aim at the restoration of coastal ecosystems.", | 74 | aim at the restoration of coastal ecosystems.", | ||
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| 209 | "subject": "Earth and Environmental Sciences", | 209 | "subject": "Earth and Environmental Sciences", | ||
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| 212 | "display_name": "The dataset supporting Chapter 4 of the PhD | 212 | "display_name": "The dataset supporting Chapter 4 of the PhD | ||
| 213 | Thesis of Roeland C. van de Vijsel httpsdoi.org10.33612", | 213 | Thesis of Roeland C. van de Vijsel httpsdoi.org10.33612", | ||
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| 215 | "name": "The dataset supporting Chapter 4 of the PhD Thesis of | 215 | "name": "The dataset supporting Chapter 4 of the PhD Thesis of | ||
| 216 | Roeland C. van de Vijsel httpsdoi.org10.33612", | 216 | Roeland C. van de Vijsel httpsdoi.org10.33612", | ||
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| 221 | "title": "Chapter 4 - Algal-induced biogeomorphic feedbacks lay the | 221 | "title": "Chapter 4 - Algal-induced biogeomorphic feedbacks lay the | ||
| 222 | groundwork for coastal wetland development", | 222 | groundwork for coastal wetland development", | ||
| 223 | "type": "dataset", | 223 | "type": "dataset", | ||
| 224 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.sc", | 224 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.sc", | ||
| t | 225 | "version": "1" | t | 225 | "version": "2" |
| 226 | } | 226 | } |