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1991) has previously modelled knick point retreat by linear diffusion and defined a response distance similar to this concept. ~o~ r 101 time [yearsl Fig. 3. Plots of incision distance x against time for various values of K, the sediment transfer coefficient, as computed from Equation (3). FLUVIAL INCISION AND SEQUENCE STRATIGRAPHY 30- 25- 29 100- IK = 1000 m2 a'll run 3 run 2 run 3 l~=,oooom2a_lI 8o- 6 2 2O- run 6 15,- run 5 ~ / / / ~ 10- ~ run 9 20run 8 20 t 000 ' 40tO00 601000 80tO00 i t O0 000 0 0 I 20 000 time, t (years) I ] 40 000 60 000 time, t (years) i 80 000 "1 1O0 000 Fig.

The river profile length was 1000 km. The horizontal broken line marks the incision distance observed for the latest Pleistocene sea level fall for the Mississippi (350 km at Baton Rouge; after Saucier 1981; Autin et al. 1991). The K value at 100 000 years is close to Kenyon & Turcotte's (1985) estimate of 560 000 m 2 a I. the river mouth would greatly affect knickpoint migration. In the examples which follow, river length >> shelf length (D>>d in Fig. 1), such that the migration of the knickpoint is not affected by the upper boundary.

JERVEY,M. T. & VAIL, P. R. 1988. Eustatic controls on clastic deposition I - conceptual framework. In: WILGUS, C. , HASTINGS,B. , KENDALL,C. G. ST. , POSAMENTIER, H. , Ross, C. A. & VAN WAGONER, J. C. (eds). Sea-level Changes: an Integrated Approach. Society of Economic Paleontologists and Mineralogists, Special Publications, 42, 109-124. READ, W. A. 1991. The Millstone Grit (Namurian) of the southern Pennines viewed in the light of eustatically controlled sequence stratigraphy. Geological Journal, 26, 167-165.

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A monograph of the Ithomiidae (Lepidoptera) Part IV: The tribe Napeogenini Fox, (American Entomological Institute. Memoir) by Richard M Fox


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