100 Years of benthic foraminiferal history on the inner Texas shelf inferred from fauna and stable isotopes: Preliminary results from two cores

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• 作者：Josiah Strauss^a ; ^b ; ^{josiahstrauss@gmail.com} ; Ethan L. Grossman^b ; Joseph A. Carlin^c ; Timothy M. Dellapenna^c
• 关键词：Foraminifera ; Stable isotopes ; Hypoxia ; Gulf of Mexico ; Coastal processes
• 刊名：Continental Shelf Research
• 出版年：2012
• 出版时间：15 April, 2012
• 年：2012
• 卷：38
• 期：Complete
• 页码：89-97
• 全文大小：714 K

文摘

Coastal regions, such as the Texas-Louisiana shelf, are subject to seasonal hypoxia that strongly depends on the magnitude of freshwater discharge from local and regional river systems. We have determined benthic foraminiferal fauna and isotopic compositions in two ²¹⁰Pb dated box cores (BR4 and BR5) to examine the evidence for nearshore hypoxia and freshwater discharge on the Texas shelf during the last 100 years. The ²¹⁰Pb chronologies of both cores reveal sedimentation rates of 0.2 and 0.1 cm yr^?, translating to ?0 and ?0 year records. The fauna of both cores were almost exclusively composed of Ammonia parkinsoniana and Elphidium excavatum, indicating euryhaline ambient waters. The Ammonia-Elphidium (A-E) index, a qualitative measure of low oxygen conditions, shows an increase from values between 20 and 50 to near 100 in both cores, suggesting low oxygen conditions between 1960 and the core top. Between 1950 and 1960 (9-10 cm), low A-E values in BR4 coincide with high ¦Ä¹⁸O and ¦Ä¹³C values greater than 0?and ??respectively. This event corresponds to severe drought (the Texas Drought of Record) over the Brazos River drainage basin and considerably reduced river discharge from 1948 to 1957. High A-E values prior to this event imply low-oxygen conditions were prevalent prior to anthropogenic exacerbation of Louisiana shelf hypoxia and at least since the dredging of a new Brazos River delta in 1929. Elphidium excavatum ¦Ä¹³C values are very low (?? and indicative of significant vital effect. The ¦Ä¹³C values of A. parkinsoniana average ??and exhibit little variability, most likely reflecting pore waters influenced by aerobic and anaerobic respiration. The association of lowered Brazos River discharge with more oxygenated shelf bottom waters suggests Brazos River discharge and shelf hypoxia are linked, but the influence of Mississippi-Atchafalaya discharge can also contribute to shelf stratification.