The Significance of Pleistocene Psilonichnu. at Willapa Bay, Washington
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Résumé
Other| April 01, 2000 The Significance of Pleistocene Psilonichnu. at Willapa Bay, Washington MURRAY K. GINGRAS; MURRAY K. GINGRAS 1The Ichnology Research Group, 1-26 E.S.B., University of Alberta, Edmonton, Alberta T6G 2E3, Canada Search for other works by this author on: GSW Google Scholar STEPHEN M. HUBBARD; STEPHEN M. HUBBARD 1The Ichnology Research Group, 1-26 E.S.B., University of Alberta, Edmonton, Alberta T6G 2E3, Canada Search for other works by this author on: GSW Google Scholar S. GEORGE PEMBERTON; S. GEORGE PEMBERTON 1The Ichnology Research Group, 1-26 E.S.B., University of Alberta, Edmonton, Alberta T6G 2E3, Canada Search for other works by this author on: GSW Google Scholar TOM SAUNDERS TOM SAUNDERS 1The Ichnology Research Group, 1-26 E.S.B., University of Alberta, Edmonton, Alberta T6G 2E3, Canada Search for other works by this author on: GSW Google Scholar PALAIOS (2000) 15 (2): 142–151. https://doi.org/10.1669/0883-1351(2000)015<0142:TSOPPA>2.0.CO;2 Article history accepted: 06 Jan 2000 first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation MURRAY K. GINGRAS, STEPHEN M. HUBBARD, S. GEORGE PEMBERTON, TOM SAUNDERS; The Significance of Pleistocene Psilonichnu. at Willapa Bay, Washington. PALAIOS 2000;; 15 (2): 142–151. doi: https://doi.org/10.1669/0883-1351(2000)015<0142:TSOPPA>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPALAIOS Search Advanced Search Abstract Two types of ichnofossils from Pleistocene outcrop at Willapa Bay are described. Because both trace fossils are characterized by an inclined to horizontal tunnel, are unlined, have an exaggerated J-shaped morphology, rarely branch, and have an unconstricted apertural opening, they have been classified as Psilonichnus upsilo. Type A and B.Psilonichnus upsilo. Type A is generally 1 to 3 cm in diameter and is infilled with laminated sediment. In general, P. upsilo. Type A is observed in ancient point-bar deposits. It has an extremely simple architecture that is almost identical to that produced by the crab Hemigrapsus oregonensi. in modern tidal flats at Willapa Bay. Psilonichnus upsilo. Type B normally exceeds 10 cm diameter and is infilled with laminated sediment. The passive infill commonly is deposited in couplets and may be delivered to the burrow network by tide-generated currents. Psilonichnus upsilo. Type B is observed in intertidal flat deposits. The overall morphology of this trace fossil is most similar to burrows generated by large crustaceans such as crabs, stomatopods, and lobsters.The occurrence of these traces leads to four findings: (1) Psilonichnus upsilo. has a more variable architecture than discussed in the literature. The size and angle of the tunnel are variable, and Psilonichnu. may aggrade, forming Teichichnu.-like structures. (2) In the modern bay, burrowing shrimp dominate subtidal, point-bar, and intertidal deposits. The Pleistocene record indicates that burrowing crabs sometimes occupied similar niches in the ancient bay. (3) Laminated, heterolithic burrow fills provide evidence of rhythmic sedimentation. These laminae represent tidal or episodic sedimentation and provide the only evidence of such processes in otherwise muddy deposits. (4) A large burrowing crab that might make P. upsilo. Type B may not be present in the modern bay. However, such a trace maker was present when these Pleistocene deposits accumulated. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,000 | 0,000 |
| Études des sciences et des technologies | 0,000 | 0,000 |
| Communication savante | 0,000 | 0,000 |
| Science ouverte | 0,000 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,019 | 0,001 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découle