2007
DOI: 10.1016/j.gca.2007.05.025
|View full text |Cite
|
Sign up to set email alerts
|

Constraining initial 230Th activity in incrementally deposited, biogenic aragonite from the Bahamas

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
7
0

Year Published

2008
2008
2018
2018

Publication Types

Select...
6
1

Relationship

3
4

Authors

Journals

citations
Cited by 8 publications
(7 citation statements)
references
References 56 publications
0
7
0
Order By: Relevance
“…Radiocarbon ratios were corrected15 for isotope fractionation using both stable isotope measurements. Age models based on 230 Th in‐growth in sclerosponge aragonite16 were used to calculate age‐corrected Δ 14 C 15. These values are compared with values measured by conventional carbonate acid digestion methodology corrected to the same age models.…”
Section: Resultsmentioning
confidence: 99%
“…Radiocarbon ratios were corrected15 for isotope fractionation using both stable isotope measurements. Age models based on 230 Th in‐growth in sclerosponge aragonite16 were used to calculate age‐corrected Δ 14 C 15. These values are compared with values measured by conventional carbonate acid digestion methodology corrected to the same age models.…”
Section: Resultsmentioning
confidence: 99%
“…For the sclerosponge, the chronology was derived solely from U/Th ages, which were measured at nine different locations in the sclerosponge skeleton and corrected for initial 230 Th incorporation following Rosenheim et al . []. The amount of initial 230 Th incorporation was estimated with the aid of two chronological constraints present in the sclerosponge skeleton: (1) the known age at the surface (2003) and (2) the location where bomb 14 C was initially present in the skeleton, which must have occurred after 1955 (when bomb 14 C was initially present in the atmosphere).…”
Section: Methodsmentioning
confidence: 99%
“…For regional comparison, sclerosponges (C. nicholsoni) from different depths in Exuma Sound, Bahamas ( Fig. 1) were also analyzed, using U/Th dates for chronology (Rosenheim et al, 2007) because these sclerosponges were too deep for fluorochrome staining by scuba divers. They were collected by submersible between 1992 and 1995 at depths ranging between 67 and 136 m. For comparison of isotope records from the same site in Jamaica, a specimen of zooxanthellate coral Montastraea faveolata was also taken from the top of the cryptic reef enclosure (14 m depth) in which the sclerosponges grew.…”
Section: Sclerosponge and Coral Sample Recoverymentioning
confidence: 99%
“…In all sclerosponges, samples mixed both pseudo-calyx Table 1 Sclerosponge sampling information. Extension rates were calculated by measuring calcein bands (PTB) or from U/Th chronology (LSI sclerosponges, Rosenheim et al, 2007). The difference between conventional and incremental depth transects is explained in the text.…”
Section: Skeletal Sub-samplingmentioning
confidence: 99%