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12-07-2001, 01:08 PM | #1 | |
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Questions for "In His Name"
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However, I'm going to give you a fair chance to prove me wrong. In my next post, I will give you several thoroughly documented biostratigraphic "case studies," and you can explain to me how the Flood explains the distribution of fossils in the geologic record. I'll start out with two simple but unequivocal lines of evidence refuting the flood theory: dessication cracks and evaporites. Even someone with little or no knowledge of the subject, such as yourself, can see plainly that neither could form during a subaqeous global deluge. A few more observations unequivocally refuting the flood "theory" include <a href="http://www.geocities.com/earthhistory/forests.htm" target="_blank">fossil forests </a>, <a href="http://www.geocities.com/earthhistory/paleosols.htm" target="_blank">stacked paleosols</a>, <a href="http://www.geocities.com/earthhistory/eggs.htm" target="_blank">dinosaur nests</a>, <a href="http://www.geocities.com/earthhistory/aigcoal.htm" target="_blank">coal deposits</a>, <a href="http://www.geocities.com/earthhistory/sap.htm" target="_blank">weathering mantles</a>, <a href="http://www.geocities.com/earthhistory/hg.htm" target="_blank">marine hardgrounds</a>, <a href="http://www.geocities.com/earthhistory/iso.htm" target="_blank">isotopic sorting</a>, and <a href="http://www.geocities.com/earthhistory/reef.htm" target="_blank">fossil reefs,</a> among many others. If you disagree, then take your pick from any of the arguments above, and we can discuss it in detail. You guys (most or all) believe that a layer strata is X amount of years. I see the evidence from Mount St Helen as evidence that shows error in popular dating methods. Well, you're in error. Your claim that "the evidence from Mount St Helen as evidence that shows error in popular dating methods" is complete nonsense, and demonstrates that you have no idea how geologic formations are dated. I've read several papers on the geologic effects of St Helens, including those written by YECs Austin, Coffin, and others, and I can say outright that the evidence from St Helens poses no such challenge. Before I go on this particular subject, perhaps you could explain the logic behind your statement. More later, Patrick [ December 07, 2001: Message edited by: ps418 ]</p> |
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12-07-2001, 01:23 PM | #2 |
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Good post. Once again you swat flies using a cannon.
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12-07-2001, 05:14 PM | #3 |
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Well, Patrick could also be said to open creationist watermellon with an axe. Good job.
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12-07-2001, 05:41 PM | #4 |
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Now for some concrete examples of the arrangement of fossils in the geologic record. Any hypothesis purporting to explain the geologic record must explain these basic data. In His Name , I would like you to enlighten us as to how "flood geology" explains this data, at least in principle.
Example 1: Neogene marine microfossils Planktonic marine protists make excellent index fossils, since they have wide distributions but short time ranges. Foraminifera and coccoliths are widely used index fossils. There are a gazillion varieties of them in the geologic record. They're not randomly mixed-up, and they're not hydraulically or ecologically sorted either, but they do occur in a definite successional order. Glenn Morton has a page listing some information on the subject. See <a href="http://www.glenn.morton.btinternet.co.uk/micro.htm" target="_blank">Microfossil Stratigraphy Presents Problems for the Flood. </a> Glenn uses the Gulf of Mexico as a reference section. Below is a list of bethic forams, planktonic forams, and nannofossils in the order they are found in Neogene sediments in the Gulf of Mexico: AGE m.y. 0.10 Globoratalia flexusa acme 0.25 Pseudoemiliania lacunosa A 0.50 "Globorot, truncatulinoides coil change R/L" 0.55 Pseudoemiliania lacunosa B 0.60 0.80 P. lacunosa variety 1.02 Sphaeroidinella dehiscens acme A P. lacunosa C 1.19 Geophyrocapsa large 1.35 Hyalinea balthica Helicosphaera sellii 1.45 Angulogerina B 1.55 Sphaeroidinella dehiscens acme B. Calcidiscus macintyrei 1.95 Discoaster brouweri 2.02 Cristellaria S 2.10 Globorotalia crassiformis Discoaster brouweri A 2.20 Globorotalia menardii coil change L/R 2.25 Lenticulina 1 2.30 Globorotalia miocenica Discoaster pentaradiatus 2.55 Discoaster surculus 3.00 Globorotalia multicamerata 3.09 Globoquadrina altispira Discoaster tamalis 3.12 Sphaeroidinellopsis seminulina 3.47 Sphenolithus abies 3.58 "Globorot, margaritae" 3.64 Reticulofenestra pseudoumbilica 4.18 Globigerina nepenthes 4.30 Sphenolithus abies B 4.38 "Buliminella 1/Tex. mexicana Amaurolithus tricorniculatus 4.90 Globigerinoides mitra Ceratolithus acutus 5.10 Textularia X 5.10 G. menardi coil change R/L 5.20 Discoaster A 5.30 Discoaster quinqueramus 5.92 Discoaster B 6.00 Discoaster Berggrenii 6.15 Robulus E 6.38 Discoaster C 6.91 Bigenerina A 7.27 Discoaster neohamatus/calcaris 7.40 Discoaster loeblichii 7.50 Catinaster mexicanus 7.60 Cristellaria K 7.80 Cyclammina 3 8.80 Bolivina thalmannii Globorotalia lenguaensis Discoaster prepentaradiatus 9.10 Discorbis 12 Discoaster bollii 9.40 Discoaster hamatus 9.50 Textularia L 9.90 Catinaster coalitus 10.80 Bigenerina 2 Globorotalia mayeri 10.85 Cibicides carstensi 10.95 Uvigerina 3 11.00 Coccolithus miopelagicus 11.90 Globorotalia fohsi robusta Discoaster kugleri acme 12.00 Textularia W 12.80 Globorotalia fohsi fohsi 12.82 Discoaster sanmiguelensis 12.85 Bigenerina humblei 13.55 Cristellaria 1 Globorotalia fohsi barisanensis 13.60 Sphenolithus heteromorphus 14.80 Praeorbulina glomerosa Sphenolithus heteromorphus acme 14.90 Cibicides opima 15.47 Amphistegina B Helicosphaera ampliaperta 15.60 15.85 Robulus L 16.39 Camerina 1/Robulus mayeri 16.77 Gyroidina 9 17.00 Catapsydrax stainforthi 17.08 Sphenolithus belemnos 17.10 Catapsydrax dissimilis 17.30 Cristellaria A 18.20 Marginulina ascensionensis 18.30 Discoaster calculosus 19.50 Discoaster sanudersi 20.20 Siphonina davisi 21.50 Cristellaria R 22.90 Helicosphaera recta 23.90 Dictyococcites bisecta 24.00 Globigerina ciperoensis 24.00 Robulus A 24.20 Discorbis gravelli 24.30 Globigerina sellii 24.35 Heterostegina sp. 24.50 Cibicides jeffersonensis 24.60 Bolivina perca 24.75 Sphenolithus ciperoensis 25.05 Marginulina idiomorpha 25.25 Marginulina vaginata 25.95 Marginulina howei 26.50 Textularia 14 26.60 Camerina A 27.10 Miogypsinoides A 27.50 Sphenolithus distentus 27.75 Cibicides hazzardi 28.10 Cyclammina A 28.60 Marginulina texana 29.00 Bolivina mexicana 29.40 Sphenolithus predistentus 29.70 Nonion struma 29.90 Nodosaria blanpiedi 30.40 Textularia seligi Globigerina ampliapertura 30.60 Discoaster tani nodifer 32.20 Textularia warreni 32.30 Cibicides mississippiensis Reticulofenestra umbilica 32.40 Loxostoma B 32.80 Ericsonia formosa The important point, as Morton points out, is that this arrangement of microfossils is found not only in the Gulf of Mexico, but over hundreds of thousands of square kilometers in the oceans. For instance, off New Jersey: Discoaster. brouweri D.pentaradiatus D.surculus D. tamalis Sphenolithus abies Reticulofenestra pseudoumbilicus Ceratolithus acutus Discoaster quinqueramus Discoaster berggrenii Discoaster Loeblichiii Discoaster Bollii And the Phillipines: Globorotalia truncatulinoides Sphaeroidinella dehiscens Globorotalia menardii Globoquandrina altispira Globigerina nepenthes Globorotalia fohsi robusta Globorotalia fohsi fohsi Globigerina ciperoensis And elsewhere. While each location may have its own unique fossils in addition to these, the order of these zonal fossils is striking. "Evolutionists" have a simple explanation for such patterns -- new species of forams and coccoliths have been appearing and disappearing, since they first appeared on earth. These microfossils are only one of many examples that could be used to make the same point, for instance Jurassic ammonites and Ordovician conodonts and Cambrian trilobites, etc. What I would like for you to explain, In His Name, is how 6-day special creation and/or flood geology explains such patterns, which are ubiquitous in the geologic record. Patrick [ December 07, 2001: Message edited by: ps418 ]</p> |
12-07-2001, 06:05 PM | #5 |
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Dear Santa
Patrick has been a very good boy this year. For Christmas please could he have a new dictionary - one which includes the word "overkill". P.S. Hey Patrick - we installed a new smilie just for you! <img src="graemlins/notworthy.gif" border="0" alt="[Not Worthy]" /> |
12-07-2001, 06:14 PM | #6 |
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In His Name,
I have another example to share with you, which I am reposting from a previous post. This example uses Ordovician graptolites as illustration of the way in which fossils are arranged within the geologic record. Graptolites are an extinct form of tiny colonial organisms now thought to be related to the hemichordates. Their remains are particularly abundant in Ordovician and Silurian sediments. They disappear from the fossil record in the early Carboniferous. Some where benthic, living attached to a substrate, and some were planktonic, floating in the water column. Their "skeletons" were composed of a chitin-like protein, which is often found as carbonized impressions on bedding planes. The actual graptolite animals lived in tiny tubes called thecae. Now, on to the test case. Cuffey writes: " . . . the development of Ordovician graptolite biostratigraphy in North America provides a good case study of biostratigraphic methods based on faunal succession (Berry, 1977), and one that is independently testable (Goldman et al., 1994; Mitchell et al., 1994). Fifteen graptolite biozones have been recognized, defined, and refined by nearly a century of detailed work. Based on superpositional order, the same succession of graptolite species and zones is recognized in New York (Ruedemann, 1904, 1908, 1912, 1925, 1947; Berry, 1962, 1963, 1970; Mitchell et al., 1994; Goldman et al., 1994), Quebec (Riva, 1969, 1974), Newfoundland (Kindle & Whittington, 1958; Whittington & Kindle, 1 963), west Texas (King, 1937; Berry, 1960; Bergstrom, 1978), Yukon (Jackson, 1964; Jackson & Lenz, 1962), and east-central Alaska (Churkin & Brabb, 1965). "Moreover, isolated localities with only short stratigraphic sections can be compared with portions of the zonation defined elsewhere (Ross & Berry, 1963). No assumption of evolution was made. The fact that this same succession occurs repeatedly in different regions all over North America, and that the succession can be independently verified by anyone willing to recollect the localities, leads to the conclusion that geochronologic correlation based on biostratigraphy is valid." The refs can be found in Cliff Cuffey's excellent article, <a href="http://www.gcssepm.org/special/cuffey_00.htm" target="_blank">The Fossil Record: Evolution or "Scientific Creation"</a> |
12-07-2001, 06:46 PM | #7 |
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And, IHN, lest you think that this succession of microfossils in the Gulf of Mexico are merely some academic waste of taxpayer's money, , may I point out that the wells that supply much of the natural gas in the US are drilled by watching which of these little critters show up in the drilled-up rock. Our old friend Bolivina mexicana, for example, shows up at about 15,000 feet subsurface just west of Rayne, Louisiana. The Monceaux #1 was drilled to look for "Bol mex", and produced 25 million cubic feet of gas per day when it found it. M. texana just wouldn't have been the same.
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12-07-2001, 07:16 PM | #8 |
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Patrick, since I rather doubt that IHN (or any other creationist for that matter) is going to address this, let me play devil's advocate (or is it Christ's advocate in this case?).
The various organisms on the bottom are simply those that are the most sensitive to disturbance, e.g., reduced oxygen levels, reduced light, increased turbidity, influx of fresh water, etc. such as would be associated with a global flood. Tougher and more tolerant organisms succumbed in the oceans, one by one, in the same succession worldwide as conditions worsened during the course of the flood. The floor is yours. |
12-07-2001, 08:58 PM | #9 | |
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Indeed, that's why the graptolites, ammonites, brachiopods, molluscs, forams and coccoliths are good examples to illustrate my point -- in these cases we're considering a succession of genera and species that clearly were similar in terms of ecological sensitivity, size, density or hydrodynamic characteristics, and ecological zonation. Although these organisms have distinct morphological characteristics that make them distinguishable as seperate genera and species, they don't possess characteristics that would account for the precise sorting we see. Let me give another vivid example. Radiolara and diatoms are both forms of marine protistans. They are roughly the same size. Both have tests (shells) made of silica. There are trillions and trillions of each in the fossil record, and therefore there must have been trillions and trillions of them in the preflood ocean. Yet while radiolarans appear in the Cambrian, diatoms do not appear until the mid-Mesozoic. But let me put some more icing on the cake -- whereas radiolara are dominantly planktonic, living near the water surface, many diatoms are benthic, leaving on the sea floor. So, the actual distribution of diatoms and radiolara is precisely the reverse of what just about any flood sorting mechanism would predict. I could go on, but let me give just one more example. There are gazillions of rugose and tabulate corals in the fossil record. There are also gazillions of scleractinian corals in the fossil record. Yet the rugosa and tabulata are present only in Paleozoic strata, while the scleractinians ar present only from the Mesozoic onwards. I'm not aware of any "flood sorting mechanism" that is not flatly contradictory to the actual distribution of fossils in the geologic record. Patrick |
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12-08-2001, 06:49 AM | #10 |
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In amplification of Patrick's posts, it's also worth noting that the sediment column in S. Louisiana is at least five miles thick. These 8000 meters are BORING sequences of delta/shallow ocean sediments, sometimes sandier, sometimes shaly. I find it rather difficult to imagine the Mississippi River bringing down that much sediment in the Flood Year, particularly when it would have to know to bring sand one day, silt the next, clay the third..... And to sort Bol mex from Marg tex at the same time? I don't think so.
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