Abstract:ABSTRACT. We report radiocarbon measurements of dissolved inorganic carbon (DIC) in surface water samples collected daily during 12 cruises to Station M in the northeast Pacific off central California. Individual surface 14 C values ranged from 22‰ to 70‰ over 10 yr. Variability of average cruise values is highest during winter likely due to increased mixing. A general decrease of 14 C values was observed at a rate of about 3‰ per year between 1994 and 2004, about half of that in atmospheric CO 2 during th… Show more
“…This average POC 14 C value is slightly lower than the average of all DIC 14 C values determined during the same study (Table 1; 47 ± 14‰; Druffel et al 2010). Model II (geometric mean) regression analysis of all average POC and DIC 14 C values resulted in a weak correlation (Figure 2; R 2 = 0.11, p = 0.0287).…”
Section: Detailed Comparison Of Poc and Dic D 14 C Signaturesmentioning
confidence: 61%
“…Surface seawater samples were collected for DIC at the same time as that for the POC samples using a bucket as described previously (Druffel et al 2010). POC particles were collected with a 33-µm mesh phytoplankton net using a clean, glass cod-end (250 mL).…”
Section: Methodsmentioning
confidence: 99%
“…A summary of individual and averaged POC 14 C values are shown together with contemporaneous DIC 14 C values (Druffel et al 2010) in both Table 1 and Figure 1. Individual 14 C values ranged from -82‰ to 66‰.…”
Section: C Signatures and Sample Pretreatment Comparisonmentioning
confidence: 99%
“…With the ultimate goal of testing the hypothesis that 14 C signatures of POC approximate those of DIC, here we report 14 C measurements of POC and DIC (Masiello et al 1998;Druffel et al 2010) samples collected from the surface water during 10 cruises from 1995-2004 in the northeast Pacific.…”
Section: Introductionmentioning
confidence: 99%
“…Here, we report ∆14C measurements of surface POC samples and compare them with contemporaneous DIC ∆14C measurements from the northeast Pacific Ocean (Hwang et al 2004;Druffel et al 2010). Samples were collected from surface waters at Station M off California between 1995 and 2004.…”
It has long been assumed that radiocarbon (∆14C) content of dissolved inorganic carbon (DIC) is equal to that of particulate organic carbon (POC) in surface seawater; however, little research has been conducted to explicitly test this assumption. Here, we report ∆14C measurements of surface POC samples and compare them with contemporaneous DIC ∆14C measurements from the northeast Pacific Ocean (Hwang et al. 2004;Druffel et al. 2010). Samples were collected from surface waters at Station M off California between 1995 and 2004. The POC ∆14C values decreased 3.2‰ per year from 1995 to 2004, similar to the decline observed in the DIC ∆14C values during the same period. Overall, our results show no statistical difference between POC and DIC ∆14C-consistent with the assumption that DIC and POC ∆14C values can generally be considered equivalent. However, significant variability was observed for POC ∆14C values during several fall/summer events, where POC ∆14C signatures were lower than DIC ∆14C values. An evaluation of 2 sample pretreatments also suggests that non-homogenized POC samples deviated less from average POC ∆14C values and more closely matched the DIC ∆14C average for the time series. The presence of seasonal POC/DIC ∆14C disagreements, combined with sample processing effects, suggest that infrequent contributions of allochthonous, older carbon may have originated from deeper in the water column, especially during periods when upwelling in this area was prominent.
“…This average POC 14 C value is slightly lower than the average of all DIC 14 C values determined during the same study (Table 1; 47 ± 14‰; Druffel et al 2010). Model II (geometric mean) regression analysis of all average POC and DIC 14 C values resulted in a weak correlation (Figure 2; R 2 = 0.11, p = 0.0287).…”
Section: Detailed Comparison Of Poc and Dic D 14 C Signaturesmentioning
confidence: 61%
“…Surface seawater samples were collected for DIC at the same time as that for the POC samples using a bucket as described previously (Druffel et al 2010). POC particles were collected with a 33-µm mesh phytoplankton net using a clean, glass cod-end (250 mL).…”
Section: Methodsmentioning
confidence: 99%
“…A summary of individual and averaged POC 14 C values are shown together with contemporaneous DIC 14 C values (Druffel et al 2010) in both Table 1 and Figure 1. Individual 14 C values ranged from -82‰ to 66‰.…”
Section: C Signatures and Sample Pretreatment Comparisonmentioning
confidence: 99%
“…With the ultimate goal of testing the hypothesis that 14 C signatures of POC approximate those of DIC, here we report 14 C measurements of POC and DIC (Masiello et al 1998;Druffel et al 2010) samples collected from the surface water during 10 cruises from 1995-2004 in the northeast Pacific.…”
Section: Introductionmentioning
confidence: 99%
“…Here, we report ∆14C measurements of surface POC samples and compare them with contemporaneous DIC ∆14C measurements from the northeast Pacific Ocean (Hwang et al 2004;Druffel et al 2010). Samples were collected from surface waters at Station M off California between 1995 and 2004.…”
It has long been assumed that radiocarbon (∆14C) content of dissolved inorganic carbon (DIC) is equal to that of particulate organic carbon (POC) in surface seawater; however, little research has been conducted to explicitly test this assumption. Here, we report ∆14C measurements of surface POC samples and compare them with contemporaneous DIC ∆14C measurements from the northeast Pacific Ocean (Hwang et al. 2004;Druffel et al. 2010). Samples were collected from surface waters at Station M off California between 1995 and 2004. The POC ∆14C values decreased 3.2‰ per year from 1995 to 2004, similar to the decline observed in the DIC ∆14C values during the same period. Overall, our results show no statistical difference between POC and DIC ∆14C-consistent with the assumption that DIC and POC ∆14C values can generally be considered equivalent. However, significant variability was observed for POC ∆14C values during several fall/summer events, where POC ∆14C signatures were lower than DIC ∆14C values. An evaluation of 2 sample pretreatments also suggests that non-homogenized POC samples deviated less from average POC ∆14C values and more closely matched the DIC ∆14C average for the time series. The presence of seasonal POC/DIC ∆14C disagreements, combined with sample processing effects, suggest that infrequent contributions of allochthonous, older carbon may have originated from deeper in the water column, especially during periods when upwelling in this area was prominent.
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