Eintrag weiter verarbeiten
Aragonite and Calcite as Constituents of Adult Oyster Shells
Gespeichert in:
| Zeitschriftentitel: | Science |
|---|---|
| Personen und Körperschaften: | |
| In: | Science, 142, 1963, 3589, S. 232-233 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
American Association for the Advancement of Science (AAAS)
|
| Schlagwörter: |
| author_facet |
Stenzel, H. B. Stenzel, H. B. |
|---|---|
| author |
Stenzel, H. B. |
| spellingShingle |
Stenzel, H. B. Science Aragonite and Calcite as Constituents of Adult Oyster Shells Multidisciplinary |
| author_sort |
stenzel, h. b. |
| spelling |
Stenzel, H. B. 0036-8075 1095-9203 American Association for the Advancement of Science (AAAS) Multidisciplinary http://dx.doi.org/10.1126/science.142.3589.232 <jats:p>Adult oyster shells are composed mainly of calcite, but there are five small areas of aragonite: the resilium, the two pads at which the adductor muscle is inserted, and the two pads at which Quenstedt's muscles are inserted. Quenstedt's muscles are proposed as a name for the small modified, one-time pedal muscles of unknown function, discovered by Quenstedt.</jats:p> Aragonite and Calcite as Constituents of Adult Oyster Shells Science |
| doi_str_mv |
10.1126/science.142.3589.232 |
| facet_avail |
Online |
| format |
ElectronicArticle |
| fullrecord |
blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTEyNi9zY2llbmNlLjE0Mi4zNTg5LjIzMg |
| id |
ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTEyNi9zY2llbmNlLjE0Mi4zNTg5LjIzMg |
| institution |
DE-Brt1 DE-D161 DE-Zi4 DE-Gla1 DE-15 DE-Pl11 DE-Rs1 DE-14 DE-105 DE-Ch1 DE-L229 DE-D275 DE-Bn3 |
| imprint |
American Association for the Advancement of Science (AAAS), 1963 |
| imprint_str_mv |
American Association for the Advancement of Science (AAAS), 1963 |
| issn |
0036-8075 1095-9203 |
| issn_str_mv |
0036-8075 1095-9203 |
| language |
English |
| mega_collection |
American Association for the Advancement of Science (AAAS) (CrossRef) |
| match_str |
stenzel1963aragoniteandcalciteasconstituentsofadultoystershells |
| publishDateSort |
1963 |
| publisher |
American Association for the Advancement of Science (AAAS) |
| recordtype |
ai |
| record_format |
ai |
| series |
Science |
| source_id |
49 |
| title |
Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_unstemmed |
Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_full |
Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_fullStr |
Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_full_unstemmed |
Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_short |
Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_sort |
aragonite and calcite as constituents of adult oyster shells |
| topic |
Multidisciplinary |
| url |
http://dx.doi.org/10.1126/science.142.3589.232 |
| publishDate |
1963 |
| physical |
232-233 |
| description |
<jats:p>Adult oyster shells are composed mainly of calcite, but there are five small areas of aragonite: the resilium, the two pads at which the adductor muscle is inserted, and the two pads at which Quenstedt's muscles are inserted. Quenstedt's muscles are proposed as a name for the small modified, one-time pedal muscles of unknown function, discovered by Quenstedt.</jats:p> |
| container_issue |
3589 |
| container_start_page |
232 |
| container_title |
Science |
| container_volume |
142 |
| format_de105 |
Article, E-Article |
| format_de14 |
Article, E-Article |
| format_de15 |
Article, E-Article |
| format_de520 |
Article, E-Article |
| format_de540 |
Article, E-Article |
| format_dech1 |
Article, E-Article |
| format_ded117 |
Article, E-Article |
| format_degla1 |
E-Article |
| format_del152 |
Buch |
| format_del189 |
Article, E-Article |
| format_dezi4 |
Article |
| format_dezwi2 |
Article, E-Article |
| format_finc |
Article, E-Article |
| format_nrw |
Article, E-Article |
| _version_ |
1792343174185746437 |
| geogr_code |
not assigned |
| last_indexed |
2024-03-01T16:47:28.976Z |
| geogr_code_person |
not assigned |
| openURL |
url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Aragonite+and+Calcite+as+Constituents+of+Adult+Oyster+Shells&rft.date=1963-10-11&genre=article&issn=1095-9203&volume=142&issue=3589&spage=232&epage=233&pages=232-233&jtitle=Science&atitle=Aragonite+and+Calcite+as+Constituents+of+Adult+Oyster+Shells&aulast=Stenzel&aufirst=H.+B.&rft_id=info%3Adoi%2F10.1126%2Fscience.142.3589.232&rft.language%5B0%5D=eng |
| SOLR | |
| _version_ | 1792343174185746437 |
| author | Stenzel, H. B. |
| author_facet | Stenzel, H. B., Stenzel, H. B. |
| author_sort | stenzel, h. b. |
| container_issue | 3589 |
| container_start_page | 232 |
| container_title | Science |
| container_volume | 142 |
| description | <jats:p>Adult oyster shells are composed mainly of calcite, but there are five small areas of aragonite: the resilium, the two pads at which the adductor muscle is inserted, and the two pads at which Quenstedt's muscles are inserted. Quenstedt's muscles are proposed as a name for the small modified, one-time pedal muscles of unknown function, discovered by Quenstedt.</jats:p> |
| doi_str_mv | 10.1126/science.142.3589.232 |
| facet_avail | Online |
| format | ElectronicArticle |
| format_de105 | Article, E-Article |
| format_de14 | Article, E-Article |
| format_de15 | Article, E-Article |
| format_de520 | Article, E-Article |
| format_de540 | Article, E-Article |
| format_dech1 | Article, E-Article |
| format_ded117 | Article, E-Article |
| format_degla1 | E-Article |
| format_del152 | Buch |
| format_del189 | Article, E-Article |
| format_dezi4 | Article |
| format_dezwi2 | Article, E-Article |
| format_finc | Article, E-Article |
| format_nrw | Article, E-Article |
| geogr_code | not assigned |
| geogr_code_person | not assigned |
| id | ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTEyNi9zY2llbmNlLjE0Mi4zNTg5LjIzMg |
| imprint | American Association for the Advancement of Science (AAAS), 1963 |
| imprint_str_mv | American Association for the Advancement of Science (AAAS), 1963 |
| institution | DE-Brt1, DE-D161, DE-Zi4, DE-Gla1, DE-15, DE-Pl11, DE-Rs1, DE-14, DE-105, DE-Ch1, DE-L229, DE-D275, DE-Bn3 |
| issn | 0036-8075, 1095-9203 |
| issn_str_mv | 0036-8075, 1095-9203 |
| language | English |
| last_indexed | 2024-03-01T16:47:28.976Z |
| match_str | stenzel1963aragoniteandcalciteasconstituentsofadultoystershells |
| mega_collection | American Association for the Advancement of Science (AAAS) (CrossRef) |
| physical | 232-233 |
| publishDate | 1963 |
| publishDateSort | 1963 |
| publisher | American Association for the Advancement of Science (AAAS) |
| record_format | ai |
| recordtype | ai |
| series | Science |
| source_id | 49 |
| spelling | Stenzel, H. B. 0036-8075 1095-9203 American Association for the Advancement of Science (AAAS) Multidisciplinary http://dx.doi.org/10.1126/science.142.3589.232 <jats:p>Adult oyster shells are composed mainly of calcite, but there are five small areas of aragonite: the resilium, the two pads at which the adductor muscle is inserted, and the two pads at which Quenstedt's muscles are inserted. Quenstedt's muscles are proposed as a name for the small modified, one-time pedal muscles of unknown function, discovered by Quenstedt.</jats:p> Aragonite and Calcite as Constituents of Adult Oyster Shells Science |
| spellingShingle | Stenzel, H. B., Science, Aragonite and Calcite as Constituents of Adult Oyster Shells, Multidisciplinary |
| title | Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_full | Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_fullStr | Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_full_unstemmed | Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_short | Aragonite and Calcite as Constituents of Adult Oyster Shells |
| title_sort | aragonite and calcite as constituents of adult oyster shells |
| title_unstemmed | Aragonite and Calcite as Constituents of Adult Oyster Shells |
| topic | Multidisciplinary |
| url | http://dx.doi.org/10.1126/science.142.3589.232 |