Matches in SemOpenAlex for { <https://semopenalex.org/work/W1980328181> ?p ?o ?g. }
- W1980328181 endingPage "4644" @default.
- W1980328181 startingPage "4627" @default.
- W1980328181 abstract "Biogenic particle reworking (234Th, Chl-a), chloropigment distributions, and pore-water irrigation rates (Br− tracer) were examined in the continental shelf-break/upper-slope region off the North Carolina, Cape Hatteras coastline. Sediment cores were obtained along three primary east–west transects (water depth ∼75–800 m; 36°20′N, 35°50′N, 35°25′N), at additional shallow stations along 35°40′N, and at slope stations within a region of complex topography known as the Manteo Lease Block. Samples were collected during August 1994, July 1996, and August 1996, and were recovered using two shipboard techniques (Haps Corer and Box Corer) as well as by the deep submersible, Johnson Sea-Link. Natural and experimental tracer distributions demonstrate that with few exceptions surface deposits throughout this region are rapidly reworked and irrigated by abundant infaunal benthos. Excess 234Th (t1/2=24.1 days) was present at all stations, with surface activities (0–0.5 cm) ranging from ∼2 to 62 dpm cm−3 (5–54 dpm g−1), average inventories of ∼28±21 (median∼24) dpm cm−2, and typical penetration depths of 5–7 cm. Steady-state particle mixing coefficients (Db) estimated using excess 234Th ranged from ∼1 to 200 cm2 yr−1. Although the highest mixing intensities were found between ∼300 and 500 m water depths, rates were locally variable, and there was little or no evidence for any consistent attenuation with bathymetric depth in either 234Th inventories or mixing intensity. Estimates of Db made using Chl-a distributions are similar to those estimated using 234Th, ranging from ∼36 to 110 cm2 yr−1. Added Br− tracer penetrated >7 cm in ∼24 h periods in shipboard-incubated sediment cores, representing rates ranging from 1.5 to 38X molecular diffusion (mean=13.1±13.0; median ∼11X). Sedimentary Chl-a and phaeophytin-a distributions below the photic zone are indicative of high input of fresh planktonic debris and rapid remineralization. These inputs presumably fuel the abundant benthic fauna, which rework sediments on the Hatteras slope at some of the highest mixing rates yet reported." @default.
- W1980328181 created "2016-06-24" @default.
- W1980328181 creator A5013351656 @default.
- W1980328181 creator A5017719758 @default.
- W1980328181 creator A5023882052 @default.
- W1980328181 creator A5032830610 @default.
- W1980328181 creator A5065060660 @default.
- W1980328181 date "2002-01-01" @default.
- W1980328181 modified "2023-09-27" @default.
- W1980328181 title "Bioturbation in shelf/slope sediments off Cape Hatteras, North Carolina: the use of 234Th, Chl-a, and Br− to evaluate rates of particle and solute transport" @default.
- W1980328181 cites W188823192 @default.
- W1980328181 cites W1966265157 @default.
- W1980328181 cites W1967153108 @default.
- W1980328181 cites W1973845975 @default.
- W1980328181 cites W1978981305 @default.
- W1980328181 cites W2008904028 @default.
- W1980328181 cites W2009730248 @default.
- W1980328181 cites W2012223181 @default.
- W1980328181 cites W2012900624 @default.
- W1980328181 cites W2014661680 @default.
- W1980328181 cites W2019342286 @default.
- W1980328181 cites W2019782908 @default.
- W1980328181 cites W2020967180 @default.
- W1980328181 cites W2029597949 @default.
- W1980328181 cites W2029940313 @default.
- W1980328181 cites W2032491023 @default.
- W1980328181 cites W2034702284 @default.
- W1980328181 cites W2036887121 @default.
- W1980328181 cites W2037104375 @default.
- W1980328181 cites W2038666455 @default.
- W1980328181 cites W2042585364 @default.
- W1980328181 cites W2044233272 @default.
- W1980328181 cites W2056036282 @default.
- W1980328181 cites W2056744700 @default.
- W1980328181 cites W2057060297 @default.
- W1980328181 cites W2064118420 @default.
- W1980328181 cites W2066641588 @default.
- W1980328181 cites W2068017679 @default.
- W1980328181 cites W2071159777 @default.
- W1980328181 cites W2074461833 @default.
- W1980328181 cites W2074752821 @default.
- W1980328181 cites W2076002163 @default.
- W1980328181 cites W2076099936 @default.
- W1980328181 cites W2076260719 @default.
- W1980328181 cites W2078328532 @default.
- W1980328181 cites W2078471503 @default.
- W1980328181 cites W2081817682 @default.
- W1980328181 cites W2084285349 @default.
- W1980328181 cites W2084710647 @default.
- W1980328181 cites W2085295538 @default.
- W1980328181 cites W2101441039 @default.
- W1980328181 cites W2109439851 @default.
- W1980328181 cites W2150448948 @default.
- W1980328181 cites W2155039073 @default.
- W1980328181 cites W2323652352 @default.
- W1980328181 cites W4231995025 @default.
- W1980328181 cites W57155991 @default.
- W1980328181 doi "https://doi.org/10.1016/s0967-0645(02)00132-7" @default.
- W1980328181 hasPublicationYear "2002" @default.
- W1980328181 type Work @default.
- W1980328181 sameAs 1980328181 @default.
- W1980328181 citedByCount "53" @default.
- W1980328181 countsByYear W19803281812012 @default.
- W1980328181 countsByYear W19803281812013 @default.
- W1980328181 countsByYear W19803281812014 @default.
- W1980328181 countsByYear W19803281812016 @default.
- W1980328181 countsByYear W19803281812017 @default.
- W1980328181 countsByYear W19803281812018 @default.
- W1980328181 countsByYear W19803281812019 @default.
- W1980328181 countsByYear W19803281812020 @default.
- W1980328181 countsByYear W19803281812022 @default.
- W1980328181 crossrefType "journal-article" @default.
- W1980328181 hasAuthorship W1980328181A5013351656 @default.
- W1980328181 hasAuthorship W1980328181A5017719758 @default.
- W1980328181 hasAuthorship W1980328181A5023882052 @default.
- W1980328181 hasAuthorship W1980328181A5032830610 @default.
- W1980328181 hasAuthorship W1980328181A5065060660 @default.
- W1980328181 hasConcept C111368507 @default.
- W1980328181 hasConcept C114793014 @default.
- W1980328181 hasConcept C117485682 @default.
- W1980328181 hasConcept C122846477 @default.
- W1980328181 hasConcept C127313418 @default.
- W1980328181 hasConcept C153018869 @default.
- W1980328181 hasConcept C174943157 @default.
- W1980328181 hasConcept C184751465 @default.
- W1980328181 hasConcept C187320778 @default.
- W1980328181 hasConcept C2816523 @default.
- W1980328181 hasConcept C39432304 @default.
- W1980328181 hasConcept C69661492 @default.
- W1980328181 hasConcept C76886044 @default.
- W1980328181 hasConcept C83042747 @default.
- W1980328181 hasConceptScore W1980328181C111368507 @default.
- W1980328181 hasConceptScore W1980328181C114793014 @default.
- W1980328181 hasConceptScore W1980328181C117485682 @default.
- W1980328181 hasConceptScore W1980328181C122846477 @default.
- W1980328181 hasConceptScore W1980328181C127313418 @default.
- W1980328181 hasConceptScore W1980328181C153018869 @default.
- W1980328181 hasConceptScore W1980328181C174943157 @default.