Changes
On October 29, 2024, 12:05:09 PM UTC,
-
Deleted resource Supplementary Table1.xlsx from Dataset belonging to "Contrasts in the marine inorganic carbon chemistry of the Benguela Upwelling System since the Last Glacial Maximum"
| f | 1 | { | f | 1 | { |
| 2 | "author": "Szabina Karancz (Royal Netherlands Institute for Sea | 2 | "author": "Szabina Karancz (Royal Netherlands Institute for Sea | ||
| 3 | Research)", | 3 | Research)", | ||
| 4 | "author_email": "szabina.karancz@nioz.nl", | 4 | "author_email": "szabina.karancz@nioz.nl", | ||
| 5 | "code": "7b.b.lh", | 5 | "code": "7b.b.lh", | ||
| 6 | "contributor": "Royal Netherlands Institute for Sea Research | 6 | "contributor": "Royal Netherlands Institute for Sea Research | ||
| 7 | (NIOZ)", | 7 | (NIOZ)", | ||
| 8 | "creator_user_id": "6f15d500-326a-48c2-a6f9-c7a3c5452234", | 8 | "creator_user_id": "6f15d500-326a-48c2-a6f9-c7a3c5452234", | ||
| 9 | "creators": | 9 | "creators": | ||
| 10 | id\":\"https://orcid.org/0000-0003-3433-3041\",\"affiliation\":\"Royal | 10 | id\":\"https://orcid.org/0000-0003-3433-3041\",\"affiliation\":\"Royal | ||
| 11 | Netherlands Institute for Sea | 11 | Netherlands Institute for Sea | ||
| 12 | tactemailaddress\":\"szabina.karancz@nioz.nl\",\"formatted\":\"Szabina | 12 | tactemailaddress\":\"szabina.karancz@nioz.nl\",\"formatted\":\"Szabina | ||
| 13 | Karancz - Royal Netherlands Institute for Sea Research - ORCID: | 13 | Karancz - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 14 | https://orcid.org/0000-0003-3433-3041 - Corresponding Author - | 14 | https://orcid.org/0000-0003-3433-3041 - Corresponding Author - | ||
| 15 | szabina.karancz@nioz.nl\"},{\"firstname\":\"Lennart J. | 15 | szabina.karancz@nioz.nl\"},{\"firstname\":\"Lennart J. | ||
| 16 | \",\"lastname\":\"de Nooijer\",\"orcid\":null,\"affiliation\":\"Royal | 16 | \",\"lastname\":\"de Nooijer\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 17 | Netherlands Institute for Sea | 17 | Netherlands Institute for Sea | ||
| 18 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Lennart | 18 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Lennart | ||
| 19 | J. de Nooijer - Royal Netherlands Institute for Sea Research - ORCID: | 19 | J. de Nooijer - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 20 | \"},{\"firstname\":\"Bas\",\"lastname\":\"van der | 20 | \"},{\"firstname\":\"Bas\",\"lastname\":\"van der | ||
| 21 | Wagt\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | 21 | Wagt\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | ||
| 22 | for Sea | 22 | for Sea | ||
| 23 | spondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Bas | 23 | spondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Bas | ||
| 24 | van der Wagt - Royal Netherlands Institute for Sea Research - ORCID: | 24 | van der Wagt - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 25 | \"},{\"firstname\":\"Marcel T. J.\",\"lastname\":\"van der | 25 | \"},{\"firstname\":\"Marcel T. J.\",\"lastname\":\"van der | ||
| 26 | Meer\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | 26 | Meer\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | ||
| 27 | for Sea | 27 | for Sea | ||
| 28 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Marcel | 28 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Marcel | ||
| 29 | T. J. van der Meer - Royal Netherlands Institute for Sea Research - | 29 | T. J. van der Meer - Royal Netherlands Institute for Sea Research - | ||
| 30 | ORCID: | 30 | ORCID: | ||
| 31 | uddha\",\"lastname\":\"Misra\",\"orcid\":null,\"affiliation\":\"Indian | 31 | uddha\",\"lastname\":\"Misra\",\"orcid\":null,\"affiliation\":\"Indian | ||
| 32 | Institute of | 32 | Institute of | ||
| 33 | ngauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Sambuddha | 33 | ngauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Sambuddha | ||
| 34 | Misra - Indian Institute of Science - ORCID: | 34 | Misra - Indian Institute of Science - ORCID: | ||
| 35 | ick\",\"lastname\":\"Hennekam\",\"orcid\":null,\"affiliation\":\"Royal | 35 | ick\",\"lastname\":\"Hennekam\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 36 | Netherlands Institute for Sea | 36 | Netherlands Institute for Sea | ||
| 37 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Rick | 37 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Rick | ||
| 38 | Hennekam - Royal Netherlands Institute for Sea Research - ORCID: | 38 | Hennekam - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 39 | Zeynep\",\"lastname\":\"Erdem\",\"orcid\":null,\"affiliation\":\"Royal | 39 | Zeynep\",\"lastname\":\"Erdem\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 40 | Netherlands Institute for Sea | 40 | Netherlands Institute for Sea | ||
| 41 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Zeynep | 41 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Zeynep | ||
| 42 | Erdem - Royal Netherlands Institute for Sea Research - ORCID: | 42 | Erdem - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 43 | ",\"lastname\":\"Lattaud\",\"orcid\":null,\"affiliation\":\"University | 43 | ",\"lastname\":\"Lattaud\",\"orcid\":null,\"affiliation\":\"University | ||
| 44 | of | 44 | of | ||
| 45 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Julie | 45 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Julie | ||
| 46 | Lattaud - University of Basel - ORCID: | 46 | Lattaud - University of Basel - ORCID: | ||
| 47 | egar\",\"lastname\":\"Haghipour\",\"orcid\":null,\"affiliation\":\"ETH | 47 | egar\",\"lastname\":\"Haghipour\",\"orcid\":null,\"affiliation\":\"ETH | ||
| 48 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Negar | 48 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Negar | ||
| 49 | Haghipour - ETH Zurich - ORCID: | 49 | Haghipour - ETH Zurich - ORCID: | ||
| 50 | fan\",\"lastname\":\"Schouten\",\"orcid\":null,\"affiliation\":\"Royal | 50 | fan\",\"lastname\":\"Schouten\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 51 | Netherlands Institute for Sea | 51 | Netherlands Institute for Sea | ||
| 52 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Stefan | 52 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Stefan | ||
| 53 | Schouten - Royal Netherlands Institute for Sea Research - ORCID: | 53 | Schouten - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 54 | Jan\",\"lastname\":\"Reichart\",\"orcid\":null,\"affiliation\":\"Royal | 54 | Jan\",\"lastname\":\"Reichart\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 55 | Netherlands Institute for Sea | 55 | Netherlands Institute for Sea | ||
| 56 | ingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Gert-Jan | 56 | ingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Gert-Jan | ||
| 57 | Reichart - Royal Netherlands Institute for Sea Research - ORCID: | 57 | Reichart - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 58 | \"}]", | 58 | \"}]", | ||
| 59 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.lh", | 59 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.lh", | ||
| 60 | "deposit_date": "2024-06-21", | 60 | "deposit_date": "2024-06-21", | ||
| 61 | "depositor": "Szabina Karancz (szabina.karancz@nioz.nl)", | 61 | "depositor": "Szabina Karancz (szabina.karancz@nioz.nl)", | ||
| 62 | "distribution_date": "2024-06-21", | 62 | "distribution_date": "2024-06-21", | ||
| 63 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 63 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 64 | Institute for Sea Research)", | 64 | Institute for Sea Research)", | ||
| 65 | "doi_date_published": "2024-06-21T10:58:31.8851524", | 65 | "doi_date_published": "2024-06-21T10:58:31.8851524", | ||
| 66 | "groups": [], | 66 | "groups": [], | ||
| 67 | "id": "8e9ffdb0-2cf6-488d-bab9-57dae70f6666", | 67 | "id": "8e9ffdb0-2cf6-488d-bab9-57dae70f6666", | ||
| 68 | "isopen": true, | 68 | "isopen": true, | ||
| 69 | "license_id": "CC0-1.0", | 69 | "license_id": "CC0-1.0", | ||
| 70 | "license_title": "CC0 1.0", | 70 | "license_title": "CC0 1.0", | ||
| 71 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | 71 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | ||
| 72 | "maintainer": "Szabina", | 72 | "maintainer": "Szabina", | ||
| 73 | "maintainer_email": "szabina.karancz@nioz.nl", | 73 | "maintainer_email": "szabina.karancz@nioz.nl", | ||
| 74 | "metadata_created": "2024-10-22T18:03:23.690031", | 74 | "metadata_created": "2024-10-22T18:03:23.690031", | ||
| n | 75 | "metadata_modified": "2024-10-29T12:05:08.333290", | n | 75 | "metadata_modified": "2024-10-29T12:05:08.660056", |
| 76 | "name": "dataset-belonging-to-", | 76 | "name": "dataset-belonging-to-", | ||
| 77 | "notes": "Upwelling regions are dynamic systems where relatively | 77 | "notes": "Upwelling regions are dynamic systems where relatively | ||
| 78 | cold, nutrient- and CO2-rich waters reach to the surface from the | 78 | cold, nutrient- and CO2-rich waters reach to the surface from the | ||
| 79 | deep. CO2 sink or source properties of these regions are dependent not | 79 | deep. CO2 sink or source properties of these regions are dependent not | ||
| 80 | only on the dissolved inorganic carbon content of the upwelled waters, | 80 | only on the dissolved inorganic carbon content of the upwelled waters, | ||
| 81 | but also on the efficiency of the biological carbon pump that provides | 81 | but also on the efficiency of the biological carbon pump that provides | ||
| 82 | constraint on the drawdown of pCO2 in the surface waters. The Benguela | 82 | constraint on the drawdown of pCO2 in the surface waters. The Benguela | ||
| 83 | Upwelling System (BUS) is a major upwelling region with one of the | 83 | Upwelling System (BUS) is a major upwelling region with one of the | ||
| 84 | most productive marine ecosystems today. However, contrasting signals | 84 | most productive marine ecosystems today. However, contrasting signals | ||
| 85 | reported on the variation in upwelling intensities based on, for | 85 | reported on the variation in upwelling intensities based on, for | ||
| 86 | instance, foraminiferal and radiolarian indices from this region over | 86 | instance, foraminiferal and radiolarian indices from this region over | ||
| 87 | the last glacial cycle indicate that a complete understanding of | 87 | the last glacial cycle indicate that a complete understanding of | ||
| 88 | (local) changes is currently lacking. To reconstruct changes in the | 88 | (local) changes is currently lacking. To reconstruct changes in the | ||
| 89 | CO2 history of the Northern Benguela upwelling region over the last 27 | 89 | CO2 history of the Northern Benguela upwelling region over the last 27 | ||
| 90 | ka BP, we used a box core (64PE450-BC6) and piston core (64PE450-PC8) | 90 | ka BP, we used a box core (64PE450-BC6) and piston core (64PE450-PC8) | ||
| 91 | from the Walvis Ridge. Here, we apply various temperature and | 91 | from the Walvis Ridge. Here, we apply various temperature and | ||
| 92 | pCO2-proxies, representing both surface (UK\u02b9 37, \u03b413C of | 92 | pCO2-proxies, representing both surface (UK\u02b9 37, \u03b413C of | ||
| 93 | alkenones) and intermediate depth (Mg/Ca, B/Ca, S/Mg, \u03b411B in | 93 | alkenones) and intermediate depth (Mg/Ca, B/Ca, S/Mg, \u03b411B in | ||
| 94 | planktonic foraminiferal shells) processes. Reconstructed pCO2 records | 94 | planktonic foraminiferal shells) processes. Reconstructed pCO2 records | ||
| 95 | suggest enhanced storage of carbon at depth during the last glacial | 95 | suggest enhanced storage of carbon at depth during the last glacial | ||
| 96 | maximum. The offset between \u03b413C of planktonic (high \u03b413C) | 96 | maximum. The offset between \u03b413C of planktonic (high \u03b413C) | ||
| 97 | and benthic foraminifera (low \u03b413C) suggests an evidence of a | 97 | and benthic foraminifera (low \u03b413C) suggests an evidence of a | ||
| 98 | more efficient biological carbon pump, potentially fuelled by remote | 98 | more efficient biological carbon pump, potentially fuelled by remote | ||
| 99 | and local iron supply through aeolian transport and dissolution in the | 99 | and local iron supply through aeolian transport and dissolution in the | ||
| 100 | shelf regions, effectively preventing release of the stored glacial | 100 | shelf regions, effectively preventing release of the stored glacial | ||
| 101 | CO2.", | 101 | CO2.", | ||
| n | 102 | "num_resources": 2, | n | 102 | "num_resources": 1, |
| 103 | "num_tags": 10, | 103 | "num_tags": 10, | ||
| 104 | "organization": { | 104 | "organization": { | ||
| 105 | "approval_status": "approved", | 105 | "approval_status": "approved", | ||
| 106 | "created": "2024-10-22T06:06:56.074257", | 106 | "created": "2024-10-22T06:06:56.074257", | ||
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| 111 | "is_organization": true, | 111 | "is_organization": true, | ||
| 112 | "name": "nioz", | 112 | "name": "nioz", | ||
| 113 | "state": "active", | 113 | "state": "active", | ||
| 114 | "title": "Royal Netherlands Institute for Sea Research", | 114 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 115 | "type": "organization" | 115 | "type": "organization" | ||
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| 171 | "subject": "Earth and Environmental Sciences", | 148 | "subject": "Earth and Environmental Sciences", | ||
| 172 | "tags": [ | 149 | "tags": [ | ||
| 173 | { | 150 | { | ||
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| 179 | }, | 156 | }, | ||
| 180 | { | 157 | { | ||
| 181 | "display_name": "Benguela Upwelling System", | 158 | "display_name": "Benguela Upwelling System", | ||
| 182 | "id": "6627773f-2967-414c-badc-58adf553ca6a", | 159 | "id": "6627773f-2967-414c-badc-58adf553ca6a", | ||
| 183 | "name": "Benguela Upwelling System", | 160 | "name": "Benguela Upwelling System", | ||
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| 192 | "vocabulary_id": null | 169 | "vocabulary_id": null | ||
| 193 | }, | 170 | }, | ||
| 194 | { | 171 | { | ||
| 195 | "display_name": "Foraminifera", | 172 | "display_name": "Foraminifera", | ||
| 196 | "id": "76541454-1cf4-41ef-bfd6-8bca9f6a5738", | 173 | "id": "76541454-1cf4-41ef-bfd6-8bca9f6a5738", | ||
| 197 | "name": "Foraminifera", | 174 | "name": "Foraminifera", | ||
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| 199 | "vocabulary_id": null | 176 | "vocabulary_id": null | ||
| 200 | }, | 177 | }, | ||
| 201 | { | 178 | { | ||
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| 204 | "name": "Inorganic carbon chemistry", | 181 | "name": "Inorganic carbon chemistry", | ||
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| 208 | { | 185 | { | ||
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| 218 | "name": "benguela upwelling system", | 195 | "name": "benguela upwelling system", | ||
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| 221 | }, | 198 | }, | ||
| 222 | { | 199 | { | ||
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| 229 | { | 206 | { | ||
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| 235 | }, | 212 | }, | ||
| 236 | { | 213 | { | ||
| 237 | "display_name": "inorganic carbon chemistry", | 214 | "display_name": "inorganic carbon chemistry", | ||
| 238 | "id": "f8f1849c-e4f9-4ca3-8eab-cf5cf6e3095b", | 215 | "id": "f8f1849c-e4f9-4ca3-8eab-cf5cf6e3095b", | ||
| 239 | "name": "inorganic carbon chemistry", | 216 | "name": "inorganic carbon chemistry", | ||
| 240 | "state": "active", | 217 | "state": "active", | ||
| 241 | "vocabulary_id": null | 218 | "vocabulary_id": null | ||
| 242 | } | 219 | } | ||
| 243 | ], | 220 | ], | ||
| 244 | "title": "Dataset belonging to \"Contrasts in the marine inorganic | 221 | "title": "Dataset belonging to \"Contrasts in the marine inorganic | ||
| 245 | carbon chemistry of the Benguela Upwelling System since the Last | 222 | carbon chemistry of the Benguela Upwelling System since the Last | ||
| 246 | Glacial Maximum\"", | 223 | Glacial Maximum\"", | ||
| 247 | "type": "dataset", | 224 | "type": "dataset", | ||
| 248 | "url": "https://doi.org/10.25850/nioz/7b.b.lh", | 225 | "url": "https://doi.org/10.25850/nioz/7b.b.lh", | ||
| 249 | "version": "1" | 226 | "version": "1" | ||
| 250 | } | 227 | } |