Research Article

Eocene (Lutetian) Shark-Rich Coastal Paleoenvironments of the Southern North Sea Basin in Europe: Biodiversity of the Marine Fürstenau Formation Including Early White and Megatooth Sharks

Figure 7

Crustacean remains and burrows from the Middle Eocene (Lutetian) gravels at Dalum. (1) Burrows by crustaceans, with large burrows of Ophiomorpha isp. and other smaller burrows in bioturbated glauconitic sands of the Fürstenau Fm. at the Osteroden sand pit (see also burrows in Figure. 3(d)). (2) Refilled Ophiomorpha isp. burrow fragment, phosphorite concretion (SCB no. Invert-41). (3) Encrusted Ophiomorpha isp. burrow fragment, phosphorite concretion (SCB no. Invert-38). (4) Refilled burrow fragment, phosphorite concretion (SCB no. Invert-40). (5) Triaxonic burrow fragment, phosphorite concretion (SCB no. Invert-39). (6) Abdomen fragment from the lobster Hoploparia  sp., phosphorite concretion (SCB no. Invert-14), dorsal. (7) Carapace of the lobster Hoploparia  sp., phosphorite concretion (SCB no. Invert-16), lateral. (8) Lower pincer of the lobster Hoploparia  sp., phosphorite concretion (SCB no. Invert-13), lateral. (9) Crab Zanthopsis large right pincer, phosphorite concretion (SCB no. Invert-18), anterior. (10) Crab Litoricola/Portunites right pincer, phosphorite concretion (SCB no. Invert-17), anterior. (11) Crab Xanthilites sp. large right pincer, phosphorite concretion (SCB no. Invert-20), anterior. (12) Crab Xanthilites sp. carapace in phosphorite concretion (SCB no. Invert-19), dorsal.
565326.fig.007