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  "author": "Daniel  Francois (Royal Netherlands Institute for Sea 
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  "author": "Daniel  Francois (Royal Netherlands Institute for Sea 
            
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Research)",
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Research)",
            
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  "author_email": "daniel.do.nascimento.silva@nioz.nl",
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  "author_email": "daniel.do.nascimento.silva@nioz.nl",
            
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  "code": "7b.b.4k",
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  "code": "7b.b.4k",
            
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  "contributor": "Royal Netherlands Institute for Sea Research 
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  "contributor": "Royal Netherlands Institute for Sea Research 
            
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(NIOZ)",
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(NIOZ)",
            
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  "creator_user_id": "f3dcb176-8da6-4bd2-b66d-a2e4e4ac121e",
            
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  "creators": "[{\"firstname\":\"Daniel\",\"lastname\":\" 
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  "creators": "[{\"firstname\":\"Daniel\",\"lastname\":\" 
            
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Francois\",\"orcid\":\"0000-0003-0173-6936\",\"affiliation\":\"Royal 
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Francois\",\"orcid\":\"0000-0003-0173-6936\",\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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ddress\":\"daniel.do.nascimento.silva@nioz.nl\",\"formatted\":\"Daniel  
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ddress\":\"daniel.do.nascimento.silva@nioz.nl\",\"formatted\":\"Daniel  
            
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Francois - Royal Netherlands Institute for Sea Research - ORCID: 
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Francois - Royal Netherlands Institute for Sea Research - ORCID: 
            
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0000-0003-0173-6936 - Corresponding Author - 
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0000-0003-0173-6936 - Corresponding Author - 
            
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daniel.do.nascimento.silva@nioz.nl\"}]",
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daniel.do.nascimento.silva@nioz.nl\"}]",
            
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  "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.4k",
            
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  "deposit_date": "2026-08-31",
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  "deposit_date": "2026-08-31",
            
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  "depositor": "Daniel do Nascimento Silva 
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  "depositor": "Daniel do Nascimento Silva 
            
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(daniel.do.nascimento.silva@nioz.nl)",
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(daniel.do.nascimento.silva@nioz.nl)",
            
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  "distribution_date": "2026-08-31",
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  "distribution_date": "2026-08-31",
            
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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": "2026-08-31T18:59:48.3661622",
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  "doi_date_published": "2026-08-31T18:59:48.3661622",
            
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  "license_title": null,
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  "license_title": null,
            
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  "maintainer": "Daniel",
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  "maintainer": "Daniel",
            
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  "maintainer_email": "daniel.do.nascimento.silva@nioz.nl",
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  "maintainer_email": "daniel.do.nascimento.silva@nioz.nl",
            
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  "metadata_created": "2026-08-31T18:35:04.505918",
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  "metadata_created": "2026-08-31T18:35:04.505918",
            
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  "metadata_modified": "2026-08-31T18:35:04.505923",
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  "metadata_modified": "2026-08-31T20:49:05.044477",
            
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  "name": "x-ray-micro-ct---foraminifera-00000001",
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  "name": "x-ray-micro-ct---foraminifera-00000001",
            
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  "notes": "Marine calcification is commonly expected to decline under 
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  "notes": "Marine calcification is commonly expected to decline under 
            
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future ocean acidification, yet the extent to which warming will 
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future ocean acidification, yet the extent to which warming will 
            
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influence this response remains unclear. We report evidence that 
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influence this response remains unclear. We report evidence that 
            
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foraminifera can sustain or enhance calcification across broad 
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foraminifera can sustain or enhance calcification across broad 
            
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pCO\u2082 (200\u20131600 ppm), particularly under warming (20\u201330 
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pCO\u2082 (200\u20131600 ppm), particularly under warming (20\u201330 
            
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\u00b0C), increasing carbonate production by up to fourfold at 
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\u00b0C), increasing carbonate production by up to fourfold at 
            
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elevated CO2 and temperature conditions. These findings highlight the 
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elevated CO2 and temperature conditions. These findings highlight the 
            
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flexibility with which foraminifera can utilize different carbon 
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flexibility with which foraminifera can utilize different carbon 
            
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sources, allowing them to increasingly benefit from the larger 
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sources, allowing them to increasingly benefit from the larger 
            
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inorganic carbon pool which is available under CO2-induced 
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inorganic carbon pool which is available under CO2-induced 
            
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acidification. Shell density was also evaluated and remained largely 
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acidification. Shell density was also evaluated and remained largely 
            
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unchanged across treatments, indicating that climate-driven responses 
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unchanged across treatments, indicating that climate-driven responses 
            
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will mainly be expressed through changes in carbonate turnover rates. 
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will mainly be expressed through changes in carbonate turnover rates. 
            
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These results suggest that temperature can offset the effects of ocean 
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These results suggest that temperature can offset the effects of ocean 
            
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acidification on calcification, with important implications for future 
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acidification on calcification, with important implications for future 
            
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marine carbonate production and thereby global carbon cycle 
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marine carbonate production and thereby global carbon cycle 
            
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feedbacks.",
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feedbacks.",
            
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  "state": "active",
            
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  "subject": "Earth and Environmental Sciences",
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  "subject": "Earth and Environmental Sciences",
            
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  "tags": [
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  "tags": [
            
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      "display_name": "biomineralisation",
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      "id": "9f1bacbc-ced2-4e04-a09e-4bb576210e68",
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      "id": "9f1bacbc-ced2-4e04-a09e-4bb576210e68",
            
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      "name": "foraminifera",
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      "name": "foraminifera",
            
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    {
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    {
            
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      "display_name": "x-ray micro-ct",
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      "display_name": "x-ray micro-ct",
            
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      "id": "3bc085a8-ae8e-4bdb-91a2-213ad6fc44e3",
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      "name": "x-ray micro-ct",
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  ],
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  "title": "X-ray micro-CT - Foraminifera",
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  "title": "X-ray micro-CT - Foraminifera",
            
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  "type": "dataset",
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  "type": "dataset",
            
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  "url": "https://doi.org/10.25850/nioz/7b.b.4k",
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  "version": "1"
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  "version": "1"
            
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}
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}