laptoppop said:
I looked for the thread before, but I didn't find it because it was in the other forum. Seems like most of the thread consists of folks patting each other on the back and congratulating themselves on how much smarter they are than the YECs. No thanks.
Rather, they noted an absence of YEC that could debate the subject on scientific grounds. Care to prove them wrong?
Now, the tread linked above also has numerous reference links in them if you want tocheck things out further.
I notice nobody is talking about the very well preserved catfish fossils -- mostly from the "18 inch layer" -- with about 4,000 layers. It is beyond reason to think that a fish could lay on the bottom of a lake for 4,000 years without decomposing so that the layers around it could gather and the fish could fossilize.
Ah, the local version of polystrate fossils? We have frequently observed this. Cold, salt, anaerobic lake water doesnt contain a lot of predators or bacteria to break down the fish
(Drever, J.I., 1997, The Geochemistry of Natural Waters, 3rd ed., Prentice Hall, Upper Saddle River, NJ)
Of course, catfish were not found throughout the system, only is specific locations (LakeGosiute only, and only the deeper center part), which speaks against them being thrown all over the place by a global flood. This specific location is also where the catfish dung fossils are found
(Grande, Lance, and H. Paul Buchheim, May, 1994, "Paleontological and Sedimentological Variation in Early Eocene Fossil Lake," Contributions to Geology, University of Wyoming, V. 30), speaking against wild, turbulent spread of fish and dung all in one place. And interestingly enough, they also found a fish who had been deposited in a layer, and animals from later layers burrowing down through the layer, right through the fish. (and of course, such a burrow cant be made until all the layers are laid down.)
And in those same layers we also find bird tracks, each in their separate layers, kind of eliminating the possibility of this having been laid down all at once
(Moussa, Mounir T., 1968, "Fossil Tracks from the Green River Formation (Eocene), Near Soldier Summit, Utah," Journal of Paleontology, 42:6:1433-1478.). And better yet, we find flamingo nesting sites, nest upon nest upon nest
(McGrew, Paul O., and Alan Feduccia 1973, "A Preliminary Report on a Nesting Colony of Eocene Birds" 25th Field Conference Wyoming Geological Association Guidebook, pp 163-165) spanning 160 meter in thickness
(Leggitt, V. Leroy, Paul H. Buchheim, and Robert E. Biaggi, 1998, "The Stratigraphic Setting of Three Presbyornis Nesting Sites: Eocene Fossil Lake, Lincoln County, Wyoming," in Vincent Santucci and Lindsay McClelland, editors National Park Service Paleontological Research, NPS/NRGRD/GRDTR-98/01 National Park Service Technical Report)
Oh, and better yet, a form of mayfly of caddisfly has yearly egg-laying sites over a 70-mile area along the past lakeshore, and in layers yearly deposited for up to 9 meters thick deposits (Leggitt, V. Leroy, and Robert A. Cushman, Jr., 2001, "Complex Caddisfly-dominated bioherms from the Eocene Green River Formation," Sedimentary Geology, 45:377-396).
The Green River varves are about 30,000 feet thick in places, and overlying another about 15-28,000 feet of sediment from non-Varve sedimentation. It also happens to be the location of the oil-shale that the US is hoping to have a future extraction process for, just to give a frame of reference.
For an idea of size, this site has a nice picture about 4 screens down. Compare with the cowsa t the bottom for size, and remember these layers were laid down with about 0.1 mm per year:
http://www.durangobill.com/Creationism.html
The Varves are made up of cyclical deposits of a few types, marl with organic compounds (low-grade oil shale), moderate-grade oil shale, or rich oil shale, and closer to the shores, fine-grained sandstone from storm runoff. In a detailed formation originally described by the first geologist to take a close look at it, (Bradley, Wilmot H., 1929, "Varves and Climate of the Green River Epoch," in USGS Professional Paper 158, p. 87-110) the 4 cyclical layers range in thickness from 0.18 mm for the sandstone to 0.16-0.037 mm for the oilshale deposits. That formation was about 2600 feet, leaving about 13 mill layers, or 3 mill+ years worth of layers (now, the thickness does vary, but the max number of varves found are about 20 mill) found at the edge of the old lake. Bradley did come back 7 years later for another survey and did find some layers as thick as 1 cm in the less oil-rich edges of the lake beds (Bradley, W.H., 1930, The varves and climate of the Green River Epoch: U.S. Geological Survey Professional Paper 158, p. 87-110.) In the center, where the catfish are, there are fewer layers, as the inflow of effluent of erosion doesnt make it that far (100 miles) and the layers truly are yearly layers without the influx of storm runoff
(Buchheim Paul H., and Robert Biaggi, "Laminae Counts Within a Synchronous Oil Shale Unit: A Challenge to the "Varve Concept," article No. 18279 referenced in GSA ABSTRACTS & PROGRAMS, 1988, v. 20, no. 7, pg. 317). These layers are also very uniform in distances of more than 100 Km
(Bradley, 1930)
The oil shale and marl came from plankton death. It is also noted that the calcium carbonate (the plankton component that turned into marl) is about 5 micron in diameter, which means that the precipitation would take quote a few days. Yet, we see cycle after cycle of these deposits. Experience with such Calcium carbonate granules tells us that the plankton itself is about 50 micron wide, and of much lighter consistency and thus settles much slower yet.
Right there, it shows that there is no possibility of a global flood of turbulent water depositing everything in one swoop.
And, of course, we also find pollen alternating in these layers, slowly sinking down and getting deposited with clay in seasonal patterns. We have directly observed such processes over the last hundred years, and also find this pattern in the varves (Richard Foster Flint, Glacial and Quaternary Geology, New York: John Wiley and Sons, Inc., 1971, p. 400.)
And we find salt layered deposits as well. Now salt layers are formed by evaporations, not floods which would dissolve the salt and spread it throughout the deposits). The area known as Wilkins peak contains numerous salt layers divided by sediment deposits from run-off So that also is a wet-dry cycle completely inconsistent with a uniform flood depositing the entire layer
(Fischer, A.G. and Roberts, L.T., Cyclicity in the Green River Formation (Lacustrine Eocene) of Wyoming," Journal of Sedimentary Petrology, vol. 61, no. 7, Dec. 1991, p. 1146-1154.)
And long-term cycles are even found. We see the difference in layers of the varves of about 5-year cycles as predicted by solar cycles as we even see today with more and less precipitation, and also a 10-15 year cycle consistent with sunspot activity cycles
(Ripepe, M, Roberts, L.T., and Fischer, A.G. 1991, "Enso and Sunspot Cycles in Varved Eocene Oil Shales from Image Analysis," Journal of Sedimentary Petrology, 61:7:1155-1163)
Fischer and Roberts,
(Fischer and Roberts, 1991) also has this interesting little bit:
" The cyclicities discussed are developed at seven levels. High-frequency cycles in the Tipton and Laney members include the annual cycle expressed in varving (1), the grouping of varves into El Nino (ENSO)-type (5.8) year cycles (2), their grouping into sunspot cycles (3), and their grouping into 30-year cycles(4). Low-frequency cycles from the Milankovitch frequency band are seen in the Tipton and Wilkins Peak members, and include the precessional 20 ka cycle (5) and the ca. 100 ka eccentricity cycle (6).
This pattern is also found in other large, deep lakes throughout the world, only in those types of lakes specifically, not in all lakes and sediment areas.
Then, of course, there are a couple of distinct layers from volcanic ash, occurring as single episodes, showing up as discrete, solid-boundary layer areas uniformly over thousands of square miles. Not exactly the smooth and uniform pattern of a global flood. O'Neill
(O'Neill, William Arthur, 1980 40Ar 39Ar ages of Selected tuffs of the Green River Formation: Wyoming, Colorado, and Utah. M.S. Thesis, OhioStateUniversity) did do dating on two such layers and found one at 46.5 mill years and another at 49.4 +/- .4 mill years. Incidentally, both were clearly defined and finite layers about 160 ft from each other, vertically,. Fitting a yearly pattern of avg. 0.1 mm deposit each year. Funny how that fits the original estimation of layers by Bradley (see above)
A quick googling of "catfish fossils green river" reveals many different explanations of the problem
Did you check out how many of them had a scientific basis?
and how the layers can easily be explained in a YEC context.
Everything can be "explained" in such a context. But there is no evidence for "explanations."