Post by 1dave on Dec 1, 2020 21:40:28 GMT -5
Determining the age of rocks -By examining tiny zircon crystals and measuring how much the original radioactive elements have converted age can be determined.
www.academia.edu/19561831/Cedar_Mountain_and_Dakota_Formations_Around_Dinosaur_National_Monument?auto=download&email_work_card=download-paper
www.academia.edu/19561831/Cedar_Mountain_and_Dakota_Formations_Around_Dinosaur_National_Monument?auto=download&email_work_card=download-paper
Age
The age of the Cedar Mountain Formation in central and southern Utah is considered
Barremian(?) to earliest Cenomanian based on dinosaur biostratigraphy (similar to the Wealden
dinosaur fauna on the Isle of Wight in southern Britain) and radiometric data (Kirkland and
others, 1997; Kirkland and others, 1999; Martill and Naish, 2001; Kirkland and Madsen, 2007;
Ward and others, 2007; Biek and others, 2010). The age of the Cedar Mountain Formation
exposed in northeastern Utah is poorly constrained. Three detrital zircons (of 63 total), dated at
104.46 ± 0.95 Ma using U-Pb analysis, indicate that the Abydosaurus mcintoshi skull bed is no
older than middle Albian at Dinosaur National Monument (Chure and others, 2010); however,
Kirkland and others (1997) have noted the Cedar Mountain Formation in central Utah is older.
In addition, Burton and others (2006) and Britt and others (2007) reported U-Pb detrital zircon
ages ranging from 124 to 109 Ma (early Aptian to middle Albian) collected at various
stratigraphic horizons from other Cedar Mountain sections in central Utah. Additional evidence
for the age comes from recent chemostratigraphic work measuring excursions of carbon isotopic
ratios from paleosols in the Cedar Mountain Formation; this new technique may have great
Current: June 6, 2012 Sprinkel, Madsen, Kirkland, Waanders, and Hunt
Original: June 1, 2005 Sprinkel-etal_CedarMtn-Dakota_06062012.docx
10
utility for dating calcareous intervals where materials used for other dating techniques are
lacking (Ludvigson and others, 2010a). Smith and others (2001), Ludvigson and others (2003b),
and Kirkland and others (2003) provide evidence for linking these excursions with known
marine carbon isotope records, based in part on work done in Dinosaur National Monument.
Chemostratigraphic evidence from the section containing the Abydosaurus mcintoshi skull bed in
the monument suggests this horizon is early Albian age (Kirkland and others, 2003; Ludvigson
and others, 2003a), in contrast to the middle Albian zircon age. A nearly 20-m-thick mudstone
separates this horizon from the lowest Dakota Formation. A recently excavated ornithopod
dinosaur skeleton from higher up section at the Reef Quarry section is currently under study; it
may be of future use in correlating these strata with other Lower Cretaceous deposits yielding
similar dinosaurs elsewhere in North America. The late Albian age of the upper Cedar Mountain
Formation is constrained by a U-Pb zircon age of 101.4 ± 0.4 Ma and middle to late Albian
palynomorphs obtained from the overlying basal Dakota Formation (see age of Dakota
Formation below and appendices D to F).
The age of the Cedar Mountain Formation in central and southern Utah is considered
Barremian(?) to earliest Cenomanian based on dinosaur biostratigraphy (similar to the Wealden
dinosaur fauna on the Isle of Wight in southern Britain) and radiometric data (Kirkland and
others, 1997; Kirkland and others, 1999; Martill and Naish, 2001; Kirkland and Madsen, 2007;
Ward and others, 2007; Biek and others, 2010). The age of the Cedar Mountain Formation
exposed in northeastern Utah is poorly constrained. Three detrital zircons (of 63 total), dated at
104.46 ± 0.95 Ma using U-Pb analysis, indicate that the Abydosaurus mcintoshi skull bed is no
older than middle Albian at Dinosaur National Monument (Chure and others, 2010); however,
Kirkland and others (1997) have noted the Cedar Mountain Formation in central Utah is older.
In addition, Burton and others (2006) and Britt and others (2007) reported U-Pb detrital zircon
ages ranging from 124 to 109 Ma (early Aptian to middle Albian) collected at various
stratigraphic horizons from other Cedar Mountain sections in central Utah. Additional evidence
for the age comes from recent chemostratigraphic work measuring excursions of carbon isotopic
ratios from paleosols in the Cedar Mountain Formation; this new technique may have great
Current: June 6, 2012 Sprinkel, Madsen, Kirkland, Waanders, and Hunt
Original: June 1, 2005 Sprinkel-etal_CedarMtn-Dakota_06062012.docx
10
utility for dating calcareous intervals where materials used for other dating techniques are
lacking (Ludvigson and others, 2010a). Smith and others (2001), Ludvigson and others (2003b),
and Kirkland and others (2003) provide evidence for linking these excursions with known
marine carbon isotope records, based in part on work done in Dinosaur National Monument.
Chemostratigraphic evidence from the section containing the Abydosaurus mcintoshi skull bed in
the monument suggests this horizon is early Albian age (Kirkland and others, 2003; Ludvigson
and others, 2003a), in contrast to the middle Albian zircon age. A nearly 20-m-thick mudstone
separates this horizon from the lowest Dakota Formation. A recently excavated ornithopod
dinosaur skeleton from higher up section at the Reef Quarry section is currently under study; it
may be of future use in correlating these strata with other Lower Cretaceous deposits yielding
similar dinosaurs elsewhere in North America. The late Albian age of the upper Cedar Mountain
Formation is constrained by a U-Pb zircon age of 101.4 ± 0.4 Ma and middle to late Albian
palynomorphs obtained from the overlying basal Dakota Formation (see age of Dakota
Formation below and appendices D to F).
Age
The age of the Cedar Mountain Formation in central and southern Utah is considered
Barremian(?) to earliest Cenomanian based on dinosaur biostratigraphy (similar to the Wealden
dinosaur fauna on the Isle of Wight in southern Britain) and radiometric data (Kirkland and
others, 1997; Kirkland and others, 1999; Martill and Naish, 2001; Kirkland and Madsen, 2007;
Ward and others, 2007; Biek and others, 2010). The age of the Cedar Mountain Formation
exposed in northeastern Utah is poorly constrained. Three detrital zircons (of 63 total), dated at
104.46 ± 0.95 Ma using U-Pb analysis, indicate that the Abydosaurus mcintoshi skull bed is no
older than middle Albian at Dinosaur National Monument (Chure and others, 2010); however,
Kirkland and others (1997) have noted the Cedar Mountain Formation in central Utah is older.
In addition, Burton and others (2006) and Britt and others (2007) reported U-Pb detrital zircon
ages ranging from 124 to 109 Ma (early Aptian to middle Albian) collected at various
stratigraphic horizons from other Cedar Mountain sections in central Utah. Additional evidence
for the age comes from recent chemostratigraphic work measuring excursions of carbon isotopic
ratios from paleosols in the Cedar Mountain Formation; this new technique may have great
Current: June 6, 2012 Sprinkel, Madsen, Kirkland, Waanders, and Hunt
Original: June 1, 2005 Sprinkel-etal_CedarMtn-Dakota_06062012.docx
10
utility for dating calcareous intervals where materials used for other dating techniques are
lacking (Ludvigson and others, 2010a). Smith and others (2001), Ludvigson and others (2003b),
and Kirkland and others (2003) provide evidence for linking these excursions with known
marine carbon isotope records, based in part on work done in Dinosaur National Monument.
Chemostratigraphic evidence from the section containing the Abydosaurus mcintoshi skull bed in
the monument suggests this horizon is early Albian age (Kirkland and others, 2003; Ludvigson
and others, 2003a), in contrast to the middle Albian zircon age. A nearly 20-m-thick mudstone
separates this horizon from the lowest Dakota Formation. A recently excavated ornithopod
dinosaur skeleton from higher up section at the Reef Quarry section is currently under study; it
may be of future use in correlating these strata with other Lower Cretaceous deposits yielding
similar dinosaurs elsewhere in North America. The late Albian age of the upper Cedar Mountain
Formation is constrained by a U-Pb zircon age of 101.4 ± 0.4 Ma and middle to late Albian
palynomorphs obtained from the overlying basal Dakota Formation (see age of Dakota
Formation below and appendices D to F).
The age of the Cedar Mountain Formation in central and southern Utah is considered
Barremian(?) to earliest Cenomanian based on dinosaur biostratigraphy (similar to the Wealden
dinosaur fauna on the Isle of Wight in southern Britain) and radiometric data (Kirkland and
others, 1997; Kirkland and others, 1999; Martill and Naish, 2001; Kirkland and Madsen, 2007;
Ward and others, 2007; Biek and others, 2010). The age of the Cedar Mountain Formation
exposed in northeastern Utah is poorly constrained. Three detrital zircons (of 63 total), dated at
104.46 ± 0.95 Ma using U-Pb analysis, indicate that the Abydosaurus mcintoshi skull bed is no
older than middle Albian at Dinosaur National Monument (Chure and others, 2010); however,
Kirkland and others (1997) have noted the Cedar Mountain Formation in central Utah is older.
In addition, Burton and others (2006) and Britt and others (2007) reported U-Pb detrital zircon
ages ranging from 124 to 109 Ma (early Aptian to middle Albian) collected at various
stratigraphic horizons from other Cedar Mountain sections in central Utah. Additional evidence
for the age comes from recent chemostratigraphic work measuring excursions of carbon isotopic
ratios from paleosols in the Cedar Mountain Formation; this new technique may have great
Current: June 6, 2012 Sprinkel, Madsen, Kirkland, Waanders, and Hunt
Original: June 1, 2005 Sprinkel-etal_CedarMtn-Dakota_06062012.docx
10
utility for dating calcareous intervals where materials used for other dating techniques are
lacking (Ludvigson and others, 2010a). Smith and others (2001), Ludvigson and others (2003b),
and Kirkland and others (2003) provide evidence for linking these excursions with known
marine carbon isotope records, based in part on work done in Dinosaur National Monument.
Chemostratigraphic evidence from the section containing the Abydosaurus mcintoshi skull bed in
the monument suggests this horizon is early Albian age (Kirkland and others, 2003; Ludvigson
and others, 2003a), in contrast to the middle Albian zircon age. A nearly 20-m-thick mudstone
separates this horizon from the lowest Dakota Formation. A recently excavated ornithopod
dinosaur skeleton from higher up section at the Reef Quarry section is currently under study; it
may be of future use in correlating these strata with other Lower Cretaceous deposits yielding
similar dinosaurs elsewhere in North America. The late Albian age of the upper Cedar Mountain
Formation is constrained by a U-Pb zircon age of 101.4 ± 0.4 Ma and middle to late Albian
palynomorphs obtained from the overlying basal Dakota Formation (see age of Dakota
Formation below and appendices D to F).