Abstract: There is a set of tidal flat deposits, with the correlated geochronological data about 1950 m.y., made of sand-silty mudstone interlayers in Changzhougou Formation of Changcheng -System in the lower part of the Upper Precambrian strata in Ming Tombs, Beijing. Many shallow water sedimentary structures can be found in the strata, such as: ripple mark, mud crack, ice model(?), runzel,rain print model, herringbone cross-bedding, flaser and lenticular bedding, etc. showing tidal flat depositional environment. It is worth noticing that among the interlayers of sand-silty mudstone there are so many burrow-like tube filling structures (See Fig.l, Fig.7, Plate I-1,2,3 and 5, Plate II 3 and 5), which have been compared by the authors with folded mud crack filling structures, ball and pillow structure, load deformation, frozen crack filling structre, sandbody liquidization structure and water escape structure, etc., but all of those sedimentary structures are helpless to interpret the genesis of the burrow-like tube filling structures in this paper. But there are many obvious similarities between the burrow-like tube filling structures and the so-called oldest Metazoan trace fossils or dubiofossils discovered by E.G Kauffman and J. R. Steidtmann in Medicine Peak Quartzite, Wyoming, U. S.A. The Medicine Peak Quartzite dated at 2000 m.y.B.P*, which is roughly coincident with the geological age of Changzhougou Formation of the Upper Precambrian Strata in Ming Tombs, Beijing. So, are these the oldest Metazoan trace fossils also? And there is also one more question- had some catastrophic events happened since 2000 m.y.B.P.to Phanerozoic so as to eliminate these oldest lives in such a long period? The authors have paid attention to the comments on the reports about the so-called oldest Metazoan trace fossils made by P.E. Cloud, H. Clemmey, J.W. Durham, and C.W. Byers, et al. It is supposed that if there was not any possibility for the existence of the oldest Metazoan trace fossils in sediments at 2000 m.y. B.P., there must be an extreme situation for the genesis of burrow-like tube filling structures either in Medicine Peak Quartzite, Wyoming or in Changzhougou Formation in Ming Tombs, Beijing. However, it is necessary for us to deal with the kinetic mechanism of burrow-like tube filling structures continuously. Fortunately, we have found a kind of traces distributed on the mudy siltstone bed surface in the middle part of Changzhougou Fr. overlaid on the layers, envoling burrow-like tube filling structures in the tidal deposits of the lower part of the Upper Precambrian Strata as mentioned above. We try to judge by the appearances of those traces as a kind of the oldest Metazoan trace fossils, according to the regular narrow grooves with two widges. The diameter of grooves is about 3mm and the widge width about 1.2mm. Those traces can be slightly straight or curved, they look very like crawled trails by some fine earthworms, however it was a long past story before 1900m.y A Canadian famous geologist, Dr.R.A. Rahmani had a look of the oldest Metazoan trace fossil on the outcrop of Changzhougou Fr. in the Ming Tombs District, when he was invited for making lectures in Beijing. Dr. R. A.Rahmani considered that was a kind of true trace fossil characterized by very regular grooves as the trace fossil Gyrochortae in Cretaceous Strata. It will be a definite support to Dr. E. G. Kauffman and Dr. J. R.Steidtmann's theory about the existence of the oldest Metazoan trace fossils in the early Proterozoic period, if the real oldest Metazoan trace fossil in the Changzhougou Fr. of the lower part of Upper Precambrian Strata (about 1900m. y. BP) in the Ming Tombs District, Beijing, China, is demonstrated.