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LDC-156.5, Fortune Bay, Newfoundland, Newfoundland and Labrador, Canada
Lat/Long (Decimal) | 47.0667,-55.8667 |
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Co-ordinates Derivation | based on nearby landmark |
Given Location | Newfoundland and Labrador, Canada |
Mindat.org Region (for given coordinates) | Fortune Bay, Newfoundland, Newfoundland and Labrador, Canada |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
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LDC-112.0, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 112.0 m, near middle of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-156.5, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the top of the regional section, at 156.5 m, near top of Member 4. | "limestone" | 530 - 520 Ma Cambrian |
LDC-39.7, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 3 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 39.7 m, in upper part of Member 3. | mudstone | 530 - 520 Ma Cambrian |
LDC-43.0, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 3 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 43.0 m, in upper part of Member 3. | mudstone | 530 - 520 Ma Cambrian |
LDC-56.6, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 3 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 56.6 m, at top of Member 3. | mudstone | 530 - 520 Ma Cambrian |
LDC-78.7, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 78.7 m, at base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-81.0, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 81.0 m, near base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-82.0, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 82.0 m, near base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-83.8, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 83.8 m, near base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-86.5, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 86.5 m, near base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-90.0, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 90.0 m, near base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-91.3, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 4 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to this as post-Nemakit-Daldynian and pre-Tommotian; Watsonella crosbyi zone; here placed in Tommotian, until clearer data are available. STRATIGRAPHIC POSITION: From the Watsonella crosbyi zone, near the middle of the regional section, at 91.3 m, near base of Member 4. | mudstone | 530 - 520 Ma Cambrian |
LDC-2.62, Fortune North [Chapel Island Fm] | Landing E., Myrow P., et al (1989) | Chapel Island | STRATIGRAPHIC RELATIONS: From Member 3 of the Chapel Island Fm, which overlies the Renconte Fm, and is overlain by the Random Fm. AGE: Unclear from Landing et al. (1989), who refers to the overlying strata as post-Nemakit-Daldynian and pre-Tommotian; "Ladatheca" cylindrica zone; here placed in Nemakit-Daldynian, until clearer data are available. STRATIGRAPHIC POSITION: From the "Ladatheca" cylindrica zone, near the base of the regional section, at 2.62 m, within upper part of Member 3. | "limestone" | 541 - 530 Ma Cambrian |
Recorded Fossils
References
Landing E., Myrow P., et al (1989) The Placentian Series: Appearance of the oldest skeletalized faunas in southeastern Newfoundland, Journal of Paleontology 63 6, 739-769 |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!