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  "code": "7b.b.ub",
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  "code": "7b.b.ub",
            
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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": "49fd5a1d-0f5a-44ab-a40a-1002a9c549e0",
            
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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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  "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.ub",
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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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entire dataset used to make all figures and do all calculations in the 
            
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manuscript \\\"van de Vijsel et al. (Submitted). Algal-induced 
            
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biogeomorphic feedbacks lay the groundwork for coastal wetland 
            
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development\\\". Final complete, finetuned version 
            
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021-09-28T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Added 
            
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\\\"Figures_JGR_Revision1_20210929.zip\\\" and 
            
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2021-10-10T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Made 
            
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dataset publicly available after manuscript was accepted for 
            
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publication in JGR 
            
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021-10-13T22:00:00.000Z\",\"type\":\"updated\",\"information\":\"Added 
            
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the DOI of the article published in JGR Biogeosciences.\"}]",
            
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  "deposit_date": "2021-03-23",
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  "deposit_date": "2021-03-23",
            
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  "depositor": "Roeland van de Vijsel",
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  "depositor": "Roeland van de Vijsel",
            
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  "distribution_date": "2021-03-23",
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  "distribution_date": "2021-03-23",
            
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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": "2021-10-11",
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  "doi_date_published": "2021-10-11",
            
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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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(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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  "license_title": "CC0 1.0",
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  "name": "7bbub",
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  "name": "7bbub",
            
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  "notes": "Coastal wetlands provide valuable ecosystem services, 
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  "notes": "Coastal wetlands provide valuable ecosystem services, 
            
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including biodiverse habitats, carbon sequestration potential and 
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including biodiverse habitats, carbon sequestration potential and 
            
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nature-based flood defense. The establishment of saltmarsh vegetation 
58
nature-based flood defense. The establishment of saltmarsh vegetation 
            
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and other key wetland species on bare tidal flats relies on windows of 
59
and other key wetland species on bare tidal flats relies on windows of 
            
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opportunity, which are traditionally linked to physical factors such 
60
opportunity, which are traditionally linked to physical factors such 
            
49
as hydrodynamic conditions, substrate stability and drainage. However, 
61
as hydrodynamic conditions, substrate stability and drainage. However, 
            
50
observations on tidal flats suggest that plant seedlings settle in 
62
observations on tidal flats suggest that plant seedlings settle in 
            
51
high densities on raised sedimentary ridges colonized by mats of 
63
high densities on raised sedimentary ridges colonized by mats of 
            
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primitive filamentous algae (Vaucheria sp.). Such algal- covered 
64
primitive filamentous algae (Vaucheria sp.). Such algal- covered 
            
53
ridges were previously shown to have higher sediment strength than 
65
ridges were previously shown to have higher sediment strength than 
            
54
substrate without algae. Here, we investigated whether these 
66
substrate without algae. Here, we investigated whether these 
            
55
measurements can be explained by physical processes only, or that 
67
measurements can be explained by physical processes only, or that 
            
56
biological (Vaucheria-induced) processes influence early saltmarsh 
68
biological (Vaucheria-induced) processes influence early saltmarsh 
            
57
establishment through the formation of stabilized bedforms. We 
69
establishment through the formation of stabilized bedforms. We 
            
58
performed two experiments under controlled mesocosm conditions, to 
70
performed two experiments under controlled mesocosm conditions, to 
            
59
test the hypotheses that i) Vaucheria grows better on elevated 
71
test the hypotheses that i) Vaucheria grows better on elevated 
            
60
topographic relief, ii) the binding force of their algal filaments 
72
topographic relief, ii) the binding force of their algal filaments 
            
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increases sediment strength, which consequently iii) maintains and 
73
increases sediment strength, which consequently iii) maintains and 
            
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creates elevated topographic relief on which algal growth is further 
74
creates elevated topographic relief on which algal growth is further 
            
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facilitated. The existence of this algal-induced biogeomorphic 
75
facilitated. The existence of this algal-induced biogeomorphic 
            
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feedback cycle was confirmed in our experiments. Our findings reveal 
76
feedback cycle was confirmed in our experiments. Our findings reveal 
            
65
that halophytic plants are not the only important ecosystem engineer 
77
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 
78
in coastal wetlands, but that fast-growing, mat- forming species like 
            
67
Vaucheria also play a major role by creating stable and elevated 
79
Vaucheria also play a major role by creating stable and elevated 
            
68
sedimentary relief. Our study indicates that biota can widen the 
80
sedimentary relief. Our study indicates that biota can widen the 
            
69
windows of opportunity for ecosystem establishment, which can be 
81
windows of opportunity for ecosystem establishment, which can be 
            
70
utilized to optimally design managed coastal realignment projects that 
82
utilized to optimally design managed coastal realignment projects that 
            
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aim at the restoration of coastal ecosystems.",
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