Hemipelagic and Pelagic Basin Plains - Trace Fossils as Indicators of Sedimentary Environments - page 674

Baldwin, C.T., McCave, I.N., 1999. Bioturbation in an active deep-sea area: implications for models
of trace fossil tiering. Palaios 14, 375-388.
Behl, R.J., 1995. Data report: detailed lithostratigraphy of Hole 893A, Santa Barbara Basin, southern
California continental borderland. In: Kennett, J.P., Baldauf, J.G., Lyle, M. (Eds.), Proc. ODP,
Scient. Res. 146, pp. 347-351.
Bentley, S.J., Sheremet, A., Jaeger, J.M., 2006. Event sedimentation, bioturbation, and preserved
sedimentary fabric: field and model comparisons in three contrasting marine settings. Cont.
Shelf Res. 26, 2108-2124.
Berger, W.H., 1982. The benthic interface of deep-sea carbonates: a three-tiered sequence controlled
by depth of deposition. In: Fanning, K.A., Manheim, F.T. (Eds.), The Dynamic Environment of
the Ocean Floor. Heath and Company, Lexington, pp. 95-114.
Berger, W.H., Heath, G.R., 1968. Vertical mixing in pelagic sediments. J. Mar. Sci. 26, 134-147.
Berger, W.H., Ekdale, A.A., Bryant, P.F., 1979. Selective preservation of burrows in deep-sea car-
bonates. Mar. Geol. 32, 205-230.
Boudreau, B.P., 1986a. Mathematics of tracer mixing in sediments. I. Spacially dependent diffusive
mixing. Am. J. Sci. 286, 161-198.
Boudreau, B.P., 1986b. Mathematics of tracer mixing in sediments. II. Nonlocal mixing and biolog-
ical conveyor belt. Am. J. Sci. 286, 199-238.
Boudreau, B.P., 1998. Mean mixed depth of sediments: the where-fore and the why. Limnol. Ocea-
nogr. 43, 524-526.
Boudreau, B., Imboden, D.M., 1987. Mathematics of tracer mixing in sediments: III. The theory of
nonlocal mixing within sediments. Am. J. Sci. 287, 693-719.
Bromley, R.G., 1991. Zoophycos : strip mine, refuse dump, cache or sewege farm? Lethaia 24,
460-462.
Bromley, R.G., Ekdale, A.A., 1984. Chondrites : a trace fossil indicator of anoxia in sediments.
Science 224, 872-874.
Bromley, R.G., Ekdale, A.A., 1986. Composite ichnofabric and tiering of burrows. Geol. Mag. 123,
49-65.
Bromley, R.G., Schulz, M.-G., Peake, N.B., 1975. Paramoudras: giant flints, long burrows and the
early diagenesis of chalk. Det Kong. Danske Vidensk. Selsk. Biol. Skr. 20, 1-31.
Byers, C.W., 1977. Biofacies Patterns inEuxinicBasins: AGeneralModel. SEPM, Spec. Publ., vol. 25,
5-17.
Chamberlain, C.K., Clark, D.L., 1973. Trace fossils and conodonts as evidence for deep-water
deposits in the Oquirrah Basin of Central Utah. J. Paleontol. 47, 663-682.
Chester, R., 2000. Marine Geochemistry. Blackwell, Oxford, 506 pp.
DeMaster, D.J., Brewster, D.C., McKee, B.A., Nittrouer, C.A., 1991. Rates of particle scavenging,
sediment reworking, and longitudinal ripple formation at the HEBBLE site based on measure-
ments of 234 Th and 210 Pb. Mar. Geol. 99, 423-444.
Edwards, B.D., 1985. Bioturbation in a dysaerobic, bathyal environment: California borderland. In:
Curran, H.A. (Ed.), Biogenic Structures: Their Use in Interpreting Depositional Environments.
SEPM Spec. Publ., vol. 35, pp. 309-331.
Ekdale, A.A., 1977. Abyssal trace fossils in worldwide deep sea drilling project cores. In:
Crimes, T.P., Harper, J.C. (Eds.), Trace Fossils 2. Geol. J., Spec. Iss. 9, pp. 163-182.
Ekdale, A.A., Bromley, R.G., 1984. Comparative ichnology of shelf-sea and deep-sea chalk.
J. Paleontol. 58, 322-332.
Ekdale, A.A., 1985. Trace fossils and mid-Cretaceous anoxic events in the Atlantic Oceans. In:
Curran, H.A. (Ed.), Biogenic Structers: Their Use in Interpreting Depositional Environments.
SEPM Spec. Publ., vol. 35, 333-342.