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Jung, M., Ilmberger, J., Mangini, A., Emeis, K.-C., 1997. Why some Mediterranean sapropels sur-
vived burn-down (and others did not). Mar. Geol. 141, 51-60.
Kakuwa, Y., 2004. Trace fossils of the Triassic to Jurassic radiolarian chert successions deposited on
the pelagic oceanic bottom. Fossils Strata 51, 58-67.
Keller, G., 1982. Organic matter and the geotechnical properties of submarine sediments. Geo-Mar.
Lett. 2, 191-198.
Konhauser, K., 2007. Introduction to Geomicrobiology. Blackwell, Oxford, 425 pp.
K ¨ nig, I., Drodt, M., Suess, E., Trautwein, A.X., 1997. Iron reduction through the tan-green color
transition in deep-sea sediments. Geochim. Cosmochim. Acta 61, 1679-1683.
Kotake, N., 1989. Paleoecology of the Zoophycos producers. Lethaia 22, 327-341.
Ksi˛ ˙ kiewicz, M., 1954. Uziarnienie frakcjonalne i laminowane we fliszu karpackim [Graded and
laminated bedding in the Carpathian Flysch]. Rocznik Pol. Tow. Geol. 22, 399-471 (in Polish).
Lampitt, R.S., Antia, A.N., 1997. Particle flux in deep seas: regional characteristics and temporal
variability. Deep-Sea Res. I 44, 1377-1403.
Laughton, A.S., 1961. Photography of the ocean floor. Ann. Rep. Smithsonian Inst. 1960, 319-326.
Legeleux, F., Reyss, J.-L., Schmidt, S., 1994. Particle mixing rates in sediments of the northeast
tropical Atlantic from 210 Pb xs ,
137 C s,
238 Th xs and 234 Th xs downcore distribution. Earth Plan.
Sci. Lett. 128, 545-562.
Leszczy´ski, S., 1993. Ichnocoenosis versus sediment colour in upper Albian to lower Eocene tur-
bidites, Guip´zcoan province, northern Spain. Palaeogeogr. Palaeoclimatol. Palaeoecol. 100,
251-265.
Leszczy´ski, S., 2004. Bioturbation structures of the Kropivnik Fucoid Marls (Campanian-lower
Maastrichtian) of the Huwniki-Rybotycze area (Polish Carpathians). Geol. Quart. 48, 35-60.
Leszczy´ski, S., Uchman, A., 1991. To the origin of variegated shales. Geol. Carp. 42, 279-289.
Leszczy´ski, S., Uchman, A., 1993. Biogenic structures of organic-poor sediments: examples from
the Paleogene variegated shales, Polish Outer Carpathians. Ichnos 2, 267-275.
Levin, L.A., Whitcraft, C.R., Mendoza, G.F., Gonzalez, J.P., Cowie, G., 2009. Oxygen and organic
matter thresholds for benthic faunal activity on the Pakistan margin oxygen minimum zone
(700-1100 m). Deep-Sea Res. II 56, 449-471.
Lobza, V., Schieber, J., 1999. Biogenic sedimentary structures produced by worms in soupy, soft
muds: observations from the Chattanooga Shale (Upper Devonian) and experiments. J. Sedi-
ment. Res. 69, 1041-1049.
Lopez, G., Taghon, G., Levinton, J.E., 1989. Ecology of Marine Deposit Feeders. Springer, Berlin,
322 pp.
L ¨ wemark, L., 2007. Importance and usefulness of trace fossils and bioturbation in paleoceanogra-
phy. In: Miller III, W. (Ed.), Trace Fossils. Concepts, Problems, Prospects. Elsevier, Amster-
dam, pp. 413-427.
L¨wemark, L., Werner, F., 2001. Dating errors in high-resolution stratigraphy: a detailed X-ray
radiograph and AMS- 14 C study of Zoophycos burrows. Mar. Geol. 177, 191-198.
L¨wemark, L., Sch¨nfeld, J., Werner, F., Sch¨fer, P., 2004. Trace fossils as a paleoceanographic
tool: evidence from Late Quaternary sediments of the southwestern Iberian margin. Mar. Geol.
204, 27-41.
L¨wemark, L., Lin, H.-L., Sarnthein, M., 2006. Temporal variations of the trace fossil Zoophycos in
a 425 ka long sediment record from the South China Sea: implications for the ethology of the
Zoophycos producer. Geol. Mag. 143, 105-114.
Lutz, M., Dunbar, R., Caldeira, K., 2002. Regional variability in the vertical flux of particulate
organic carbon in the ocean interior. Glob. Biogeochem. Cy. 16, 1037-1055.
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