Changes
On August 4, 2023 at 9:32:38 AM UTC, admin:
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Moved Pedogeomorphology, geochronology and paleobotany of soil profiles obtained in the Nagqu area, central Tibet from organization PANGEA (Agriculture) to organization PANGAEA (Agriculture)
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Changed value of field
repository_name
toPANGAEA (Data Publisher for Earth & Environmental Science)
in Pedogeomorphology, geochronology and paleobotany of soil profiles obtained in the Nagqu area, central Tibet
f | 1 | { | f | 1 | { |
2 | "author": "Kaiser Knut", | 2 | "author": "Kaiser Knut", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
5 | "doi": "10.1594/PANGAEA.787168", | 5 | "doi": "10.1594/PANGAEA.787168", | ||
6 | "doi_date_published": "2008", | 6 | "doi_date_published": "2008", | ||
7 | "doi_publisher": "", | 7 | "doi_publisher": "", | ||
8 | "doi_status": "True", | 8 | "doi_status": "True", | ||
9 | "extra_authors": [ | 9 | "extra_authors": [ | ||
10 | { | 10 | { | ||
11 | "extra_author": "Miehe Georg", | 11 | "extra_author": "Miehe Georg", | ||
12 | "orcid": "" | 12 | "orcid": "" | ||
13 | }, | 13 | }, | ||
14 | { | 14 | { | ||
15 | "extra_author": "Barthelmes Alexandra", | 15 | "extra_author": "Barthelmes Alexandra", | ||
16 | "orcid": "" | 16 | "orcid": "" | ||
17 | }, | 17 | }, | ||
18 | { | 18 | { | ||
19 | "extra_author": "Ehrmann Otto", | 19 | "extra_author": "Ehrmann Otto", | ||
20 | "orcid": "" | 20 | "orcid": "" | ||
21 | }, | 21 | }, | ||
22 | { | 22 | { | ||
23 | "extra_author": "Scharf Andreas", | 23 | "extra_author": "Scharf Andreas", | ||
24 | "orcid": "" | 24 | "orcid": "" | ||
25 | }, | 25 | }, | ||
26 | { | 26 | { | ||
27 | "extra_author": "Schult Manuela", | 27 | "extra_author": "Schult Manuela", | ||
28 | "orcid": "" | 28 | "orcid": "" | ||
29 | }, | 29 | }, | ||
30 | { | 30 | { | ||
31 | "extra_author": "Schl\u00fctz Frank", | 31 | "extra_author": "Schl\u00fctz Frank", | ||
32 | "orcid": "0000-0003-2114-8146" | 32 | "orcid": "0000-0003-2114-8146" | ||
33 | }, | 33 | }, | ||
34 | { | 34 | { | ||
35 | "extra_author": "Adamczyk Sonja", | 35 | "extra_author": "Adamczyk Sonja", | ||
36 | "orcid": "" | 36 | "orcid": "" | ||
37 | }, | 37 | }, | ||
38 | { | 38 | { | ||
39 | "extra_author": "Frenzel Burkhard", | 39 | "extra_author": "Frenzel Burkhard", | ||
40 | "orcid": "" | 40 | "orcid": "" | ||
41 | } | 41 | } | ||
42 | ], | 42 | ], | ||
43 | "groups": [], | 43 | "groups": [], | ||
44 | "id": "5ea932c1-ab73-4cef-b0dd-fc5e642fa356", | 44 | "id": "5ea932c1-ab73-4cef-b0dd-fc5e642fa356", | ||
45 | "isopen": false, | 45 | "isopen": false, | ||
46 | "license_id": "CC-BY-3.0", | 46 | "license_id": "CC-BY-3.0", | ||
47 | "license_title": "CC-BY-3.0", | 47 | "license_title": "CC-BY-3.0", | ||
48 | "metadata_created": "2023-01-12T13:31:15.938672", | 48 | "metadata_created": "2023-01-12T13:31:15.938672", | ||
n | 49 | "metadata_modified": "2023-01-12T13:31:15.938678", | n | 49 | "metadata_modified": "2023-08-04T09:32:38.751999", |
50 | "name": "png-doi-10-1594-pangaea-787168", | 50 | "name": "png-doi-10-1594-pangaea-787168", | ||
51 | "notes": "Vast areas on the Tibetan Plateau are covered by alpine | 51 | "notes": "Vast areas on the Tibetan Plateau are covered by alpine | ||
52 | sedge mats consisting of different species of the genus Kobresia. | 52 | sedge mats consisting of different species of the genus Kobresia. | ||
53 | These mats have topsoil horizons rich in rhizogenic organic matter | 53 | These mats have topsoil horizons rich in rhizogenic organic matter | ||
54 | which creates turfs. As the turfs have recently been affected by a | 54 | which creates turfs. As the turfs have recently been affected by a | ||
55 | complex destruction process, knowledge concerning their soil | 55 | complex destruction process, knowledge concerning their soil | ||
56 | properties, age and pedogenesis are needed. In the core area of | 56 | properties, age and pedogenesis are needed. In the core area of | ||
57 | Kobresia pygmaea mats around Nagqu (central Tibetan Plateau, ca. 4500 | 57 | Kobresia pygmaea mats around Nagqu (central Tibetan Plateau, ca. 4500 | ||
58 | m a.s.l.), four profiles were subjected to pedological, paleobotanical | 58 | m a.s.l.), four profiles were subjected to pedological, paleobotanical | ||
59 | and geochronological analyses concentrating on soil properties, | 59 | and geochronological analyses concentrating on soil properties, | ||
60 | phytogenic composition and dating of the turf. The turf of both dry K. | 60 | phytogenic composition and dating of the turf. The turf of both dry K. | ||
61 | pygmaea sites and wet Kobresia schoenoides sites is characterised by | 61 | pygmaea sites and wet Kobresia schoenoides sites is characterised by | ||
62 | an enrichment of living (dominant portion) and dead root biomass. In | 62 | an enrichment of living (dominant portion) and dead root biomass. In | ||
63 | terms of humus forms, K. pygmaea turfs can be classified as Rhizomulls | 63 | terms of humus forms, K. pygmaea turfs can be classified as Rhizomulls | ||
64 | mainly developed from Cambisols. Wet-site K. schoenoides turfs, | 64 | mainly developed from Cambisols. Wet-site K. schoenoides turfs, | ||
65 | however, can be classified as Rhizo-Hydromors developed from Histic | 65 | however, can be classified as Rhizo-Hydromors developed from Histic | ||
66 | Gleysols. At the dry sites studied, the turnover of soil organic | 66 | Gleysols. At the dry sites studied, the turnover of soil organic | ||
67 | matter is controlled by a non-permafrost cold thermal regime. | 67 | matter is controlled by a non-permafrost cold thermal regime. | ||
68 | Below-ground remains from sedges are the most frequent macroremains in | 68 | Below-ground remains from sedges are the most frequent macroremains in | ||
69 | the turf. Only a few pollen types of vascular plants occur, | 69 | the turf. Only a few pollen types of vascular plants occur, | ||
70 | predominantly originating from sedges and grasses. Large amounts of | 70 | predominantly originating from sedges and grasses. Large amounts of | ||
71 | microscopic charcoal (indeterminate) are present. Macroremains and | 71 | microscopic charcoal (indeterminate) are present. Macroremains and | ||
72 | pollen extracted from the turfs predominantly have negative AMS 14C | 72 | pollen extracted from the turfs predominantly have negative AMS 14C | ||
73 | ages, giving evidence of a modern turf genesis. Bulk-soil datings from | 73 | ages, giving evidence of a modern turf genesis. Bulk-soil datings from | ||
74 | the lowermost part of the turfs have a Late Holocene age comprising | 74 | the lowermost part of the turfs have a Late Holocene age comprising | ||
75 | the last ca. 2000 years. The development of K. pygmaea turfs was most | 75 | the last ca. 2000 years. The development of K. pygmaea turfs was most | ||
76 | probably caused by an anthropo(zoo)-genetically initiated growth of | 76 | probably caused by an anthropo(zoo)-genetically initiated growth of | ||
77 | sedge mats replacing former grass-dominated vegetation ('steppe'). | 77 | sedge mats replacing former grass-dominated vegetation ('steppe'). | ||
78 | Thus the turfs result from the transformation of pre-existing topsoils | 78 | Thus the turfs result from the transformation of pre-existing topsoils | ||
79 | comprising a secondary penetration and accumulation of roots. K. | 79 | comprising a secondary penetration and accumulation of roots. K. | ||
80 | schoenoides turfs, however, are characterised by a combined process of | 80 | schoenoides turfs, however, are characterised by a combined process of | ||
81 | peat formation and penetration/accumulation of roots probably | 81 | peat formation and penetration/accumulation of roots probably | ||
82 | representing a (quasi) natural wetland vegetation.", | 82 | representing a (quasi) natural wetland vegetation.", | ||
83 | "num_resources": 0, | 83 | "num_resources": 0, | ||
84 | "num_tags": 0, | 84 | "num_tags": 0, | ||
85 | "orcid": "0000-0002-5080-6075", | 85 | "orcid": "0000-0002-5080-6075", | ||
86 | "organization": { | 86 | "organization": { | ||
87 | "approval_status": "approved", | 87 | "approval_status": "approved", | ||
n | 88 | "created": "2023-01-12T13:31:15.534211", | n | 88 | "created": "2023-08-04T09:32:38.098376", |
89 | "description": "PANGEA (Data Publisher for Earth & Environmental | 89 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
90 | Science): The information system PANGAEA is operated as an Open Access | 90 | Science): The information system PANGAEA is operated as an Open Access | ||
91 | library aimed at archiving, publishing and distributing georeferenced | 91 | library aimed at archiving, publishing and distributing georeferenced | ||
92 | data from earth system research. PANGAEA guarantees long-term | 92 | data from earth system research. PANGAEA guarantees long-term | ||
93 | availability (greater than 10 years) of its content. PANGAEA is open | 93 | availability (greater than 10 years) of its content. PANGAEA is open | ||
94 | to any project, institution, or individual scientist to use or to | 94 | to any project, institution, or individual scientist to use or to | ||
95 | archive and publish data. PANGAEA focuses on georeferenced | 95 | archive and publish data. PANGAEA focuses on georeferenced | ||
96 | observational data, experimental data, and models/simulations. | 96 | observational data, experimental data, and models/simulations. | ||
97 | Citability, comprehensive metadata descriptions, interoperability of | 97 | Citability, comprehensive metadata descriptions, interoperability of | ||
98 | data and metadata, a high degree of structural and semantic | 98 | data and metadata, a high degree of structural and semantic | ||
99 | harmonization of the data inventory as well as the commitment of the | 99 | harmonization of the data inventory as well as the commitment of the | ||
100 | hosting institutions ensures FAIRness of archived data.", | 100 | hosting institutions ensures FAIRness of archived data.", | ||
n | 101 | "id": "bde9e9b1-5746-46d6-809c-7515b699dbac", | n | 101 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", |
102 | "image_url": "pangea-logo.png", | 102 | "image_url": "pangea-logo.png", | ||
103 | "is_organization": true, | 103 | "is_organization": true, | ||
n | 104 | "name": "pangea", | n | 104 | "name": "pangaea", |
105 | "state": "active", | 105 | "state": "active", | ||
n | 106 | "title": "PANGEA (Agriculture)", | n | 106 | "title": "PANGAEA (Agriculture)", |
107 | "type": "organization" | 107 | "type": "organization" | ||
108 | }, | 108 | }, | ||
n | 109 | "owner_org": "bde9e9b1-5746-46d6-809c-7515b699dbac", | n | 109 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", |
110 | "private": false, | 110 | "private": false, | ||
111 | "publication_year": "2008", | 111 | "publication_year": "2008", | ||
n | n | 112 | "related_identifiers": [ | ||
113 | { | ||||
114 | "authors": "Kaiser Knut,Miehe Georg,Barthelmes Alexandra,Ehrmann | ||||
115 | Otto,Scharf Andreas,Schult Manuela,Schl\u00fctz Frank,Adamczyk | ||||
116 | Sonja,Frenzel Burkhard", | ||||
117 | "email_authors": | ||||
118 | ,fschlue@gwdg.de,Adamczyk@uni-hohenheim.de,bfrenzel@uni-hohenheim.de", | ||||
119 | "identifier": "https://doi.org/10.1016/j.catena.2007.12.001", | ||||
120 | "identifier_type": "DOI", | ||||
121 | "orcid_authors": | ||||
122 | "0000-0002-5080-6075,,,,,,0000-0003-2114-8146,,", | ||||
123 | "relation_type": "IsSupplementTo", | ||||
124 | "source": "CATENA", | ||||
125 | "title": "Turf-bearing topsoils on the central Tibetan Plateau, | ||||
126 | China: Pedology, botany, geochronology", | ||||
127 | "year": "2008" | ||||
128 | } | ||||
129 | ], | ||||
112 | "relationships_as_object": [], | 130 | "relationships_as_object": [], | ||
113 | "relationships_as_subject": [], | 131 | "relationships_as_subject": [], | ||
n | 114 | "repository_name": "PANGEA (Data Publisher for Earth & Environmental | n | 132 | "repository_name": "PANGAEA (Data Publisher for Earth & |
115 | Science)", | 133 | Environmental Science)", | ||
116 | "resource_type": "application/zip - filename: Kaiser_2008", | 134 | "resource_type": "application/zip - filename: Kaiser_2008", | ||
117 | "resources": [], | 135 | "resources": [], | ||
t | t | 136 | "services_used_list": "", | ||
118 | "source_metadata_created": "2008", | 137 | "source_metadata_created": "2008", | ||
119 | "source_metadata_modified": "", | 138 | "source_metadata_modified": "", | ||
120 | "state": "active", | 139 | "state": "active", | ||
121 | "subject_areas": [ | 140 | "subject_areas": [ | ||
122 | { | 141 | { | ||
123 | "subject_area_additional": "", | 142 | "subject_area_additional": "", | ||
124 | "subject_area_name": "Agriculture" | 143 | "subject_area_name": "Agriculture" | ||
125 | }, | 144 | }, | ||
126 | { | 145 | { | ||
127 | "subject_area_additional": "", | 146 | "subject_area_additional": "", | ||
128 | "subject_area_name": "LakesRivers" | 147 | "subject_area_name": "LakesRivers" | ||
129 | }, | 148 | }, | ||
130 | { | 149 | { | ||
131 | "subject_area_additional": "", | 150 | "subject_area_additional": "", | ||
132 | "subject_area_name": "Lithosphere" | 151 | "subject_area_name": "Lithosphere" | ||
133 | } | 152 | } | ||
134 | ], | 153 | ], | ||
135 | "tags": [], | 154 | "tags": [], | ||
136 | "title": "Pedogeomorphology, geochronology and paleobotany of soil | 155 | "title": "Pedogeomorphology, geochronology and paleobotany of soil | ||
137 | profiles obtained in the Nagqu area, central Tibet", | 156 | profiles obtained in the Nagqu area, central Tibet", | ||
138 | "type": "vdataset", | 157 | "type": "vdataset", | ||
139 | "url": "https://doi.org/10.1594/PANGAEA.787168" | 158 | "url": "https://doi.org/10.1594/PANGAEA.787168" | ||
140 | } | 159 | } |