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  "code": "7b.b.sc",
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  "code": "7b.b.sc",
            
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
            
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  "creator_user_id": "69f9b76b-b950-4856-85f4-a7909fc0cc49",
            
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  "creators": "[{\"firstname\":\"Roeland C.\",\"lastname\":\"van de 
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  "creators": "[{\"firstname\":\"Roeland C.\",\"lastname\":\"van de 
            
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Vijsel\",\"affiliation\":\"Royal Netherlands Institute for Sea 
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Vijsel\",\"affiliation\":\"Royal Netherlands Institute for Sea 
            
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scorrespondingauthor\":true},{\"firstname\":\"Jim\",\"lastname\":\"van 
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scorrespondingauthor\":true},{\"firstname\":\"Jim\",\"lastname\":\"van 
            
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Belzen\",\"affiliation\":\"Royal Netherlands Institute for Sea 
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Belzen\",\"affiliation\":\"Royal Netherlands Institute for Sea 
            
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ddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Tjeerd 
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ddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Tjeerd 
            
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J.\",\"lastname\":\"Bouma\",\"affiliation\":\"Royal Netherlands 
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J.\",\"lastname\":\"Bouma\",\"affiliation\":\"Royal Netherlands 
            
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Institute for Sea 
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Institute for Sea 
            
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respondingauthor\":false},{\"firstname\":\"Daphne\",\"lastname\":\"van 
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respondingauthor\":false},{\"firstname\":\"Daphne\",\"lastname\":\"van 
            
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der Wal\",\"affiliation\":\"Royal Netherlands Institute for Sea 
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der Wal\",\"affiliation\":\"Royal Netherlands Institute for Sea 
            
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rrespondingauthor\":false},{\"firstname\":\"Johan\",\"lastname\":\"van 
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rrespondingauthor\":false},{\"firstname\":\"Johan\",\"lastname\":\"van 
            
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de Koppel\",\"affiliation\":\"Royal Netherlands Institute for Sea 
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de Koppel\",\"affiliation\":\"Royal Netherlands Institute for Sea 
            
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275\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]",
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275\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]",
            
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  "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.sc",
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  "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.sc",
            
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  "dates": 
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  "dates": 
            
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021-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"The 
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021-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"The 
            
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dataset supporting Chapter 4 of the PhD Thesis of Roeland C. van de 
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dataset supporting Chapter 4 of the PhD Thesis of Roeland C. van de 
            
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Vijsel (https://doi.org/10.33612/diss.160081233).\"}]",
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Vijsel (https://doi.org/10.33612/diss.160081233).\"}]",
            
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  "deposit_date": "2021-07-13",
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  "deposit_date": "2021-07-13",
            
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  "depositor": "Roeland van de Vijsel",
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  "depositor": "Roeland van de Vijsel",
            
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  "distribution_date": "2021-07-13",
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  "distribution_date": "2021-07-13",
            
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
            
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Institute for Sea Research)",
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Institute for Sea Research)",
            
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  "doi_date_published": "2023-11-22",
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  "doi_date_published": "2023-11-22",
            
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  "funding_references": "[{\"name\":\"Netherlands Organisation for 
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  "funding_references": "[{\"name\":\"Netherlands Organisation for 
            
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Scientific Research 
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Scientific Research 
            
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(NWO)\",\"awardnumber\":\"869.15.003\",\"awardtitle\":\"The New 
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(NWO)\",\"awardnumber\":\"869.15.003\",\"awardtitle\":\"The New 
            
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Delta\"},{\"name\":\"Vlaams-Nederlandse Scheldecommissie 
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Delta\"},{\"name\":\"Vlaams-Nederlandse Scheldecommissie 
            
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(VNSC)\",\"awardnumber\":\"3109 1805\",\"awardtitle\":\"Vegetation 
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(VNSC)\",\"awardnumber\":\"3109 1805\",\"awardtitle\":\"Vegetation 
            
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modelling HPP\"}]",
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modelling HPP\"}]",
            
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  "name": "7bbsc",
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  "name": "7bbsc",
            
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  "notes": "Coastal wetlands provide valuable ecosystem services, 
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  "notes": "Coastal wetlands provide valuable ecosystem services, 
            
46
including biodiverse habitats, carbon sequestration potential and 
46
including biodiverse habitats, carbon sequestration potential and 
            
47
nature-based flood defense. The establishment of saltmarsh vegetation 
47
nature-based flood defense. The establishment of saltmarsh vegetation 
            
48
and other key wetland species on bare tidal flats relies on windows of 
48
and other key wetland species on bare tidal flats relies on windows of 
            
49
opportunity, which are traditionally linked to physical factors such 
49
opportunity, which are traditionally linked to physical factors such 
            
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as hydrodynamic conditions, substrate stability and drainage. However, 
50
as hydrodynamic conditions, substrate stability and drainage. However, 
            
51
observations on tidal flats suggest that plant seedlings settle in 
51
observations on tidal flats suggest that plant seedlings settle in 
            
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high densities on raised sedimentary ridges colonized by mats of 
52
high densities on raised sedimentary ridges colonized by mats of 
            
53
primitive filamentous algae (Vaucheria sp.). Such algal-covered ridges 
53
primitive filamentous algae (Vaucheria sp.). Such algal-covered ridges 
            
54
were previously shown to have higher sediment strength than substrate 
54
were previously shown to have higher sediment strength than substrate 
            
55
without algae. Here, we investigated whether these measurements can be 
55
without algae. Here, we investigated whether these measurements can be 
            
56
explained by physical processes only, or that biological 
56
explained by physical processes only, or that biological 
            
57
(Vaucheria-induced) processes influence early saltmarsh establishment 
57
(Vaucheria-induced) processes influence early saltmarsh establishment 
            
58
through the formation of stabilized bedforms. We performed two 
58
through the formation of stabilized bedforms. We performed two 
            
59
experiments under controlled mesocosm conditions, to test the 
59
experiments under controlled mesocosm conditions, to test the 
            
60
hypotheses that i) Vaucheria grows better on elevated topographic 
60
hypotheses that i) Vaucheria grows better on elevated topographic 
            
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relief, ii) the binding force of their algal filaments increases 
61
relief, ii) the binding force of their algal filaments increases 
            
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sediment strength, which consequently iii) maintains and creates 
62
sediment strength, which consequently iii) maintains and creates 
            
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elevated topographic relief on which algal growth is further 
63
elevated topographic relief on which algal growth is further 
            
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facilitated. The existence of this algal-induced biogeomorphic 
64
facilitated. The existence of this algal-induced biogeomorphic 
            
65
feedback cycle was confirmed in our experiments. Our findings reveal 
65
feedback cycle was confirmed in our experiments. Our findings reveal 
            
66
that halophytic plants are not the only important ecosystem engineer 
66
that halophytic plants are not the only important ecosystem engineer 
            
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in coastal wetlands, but that fast-growing, mat- forming species like 
67
in coastal wetlands, but that fast-growing, mat- forming species like 
            
68
Vaucheria also play a major role by creating stable and elevated 
68
Vaucheria also play a major role by creating stable and elevated 
            
69
sedimentary relief. Our study indicates that biota can widen the 
69
sedimentary relief. Our study indicates that biota can widen the 
            
70
windows of opportunity for ecosystem establishment, which can be 
70
windows of opportunity for ecosystem establishment, which can be 
            
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utilized to optimally design managed coastal realignment projects that 
71
utilized to optimally design managed coastal realignment projects that 
            
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aim at the restoration of coastal ecosystems.",
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aim at the restoration of coastal ecosystems.",
            
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