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GEOSCIENCE REPORTS — Number 17, Winter 1994

p.1 • Catastrophes and Earth History • Leonard Brand
p.4 • Editorial
p.5 • Science News - Biology, Geology, Paleontology, Dino Notes
p.6 • GRI News
p.8 • Paleobiology of Dinosaurs • M. Elaine Kennedy


EDITORIAL

    The feature article in this issue was contributed by Dr. Leonard Brand, Chairman of the Department of Natural Sciences at Loma Linda University. The article was originally published in the department's newsletter, "Earth History News." He was kind enough to allow us to republish it for the benefit of secondary-level science teachers and their students.
    While the acceptance and recognition of catastrophic events in the geologic record represents a major shift in the thinking of geologists, there is no indication that scientists are willing to consider the validity of a worldwide catastrophe such as the Noachian flood (see Brand's comments on Bretz, this issue). Allen and Bums, in their book Cataclysms on the Columbia (Timber Press, 1986), state, "Bretz's opponents saw only what they had resolved to see. They were prime examples of the geologic quip, 'I wouldn't have seen it, if I hadn't believed it.' Like members of a faith whose existence is threatened when one small variant is thrown into the system, so these men seemed to feel the entire discipline of geology, and all it stood for, would be sent crashing if Bretzs reintrepretation of catastrophism. were given serious consideration. " Attitudes toward creationi d flood geology seem little changed from Bretzs day. However, the geologic record of Catastrophes is consistent with the biblical account of a very complex, worldwide flood, with an aftermath extending well beyond the flood year.
    We want to thank Dr. Brand for his willingness to contribute to Geoscience Reports.

 

SCIENCE NEWS

BIOLOGY

Jablonka, E., M. Lachmann and M. J. Lamb. 1992. Evidence, mechanisms and models for the inheritance of acquired characters. Journal of Theoretical Biology 158:245-268.

    Proper gene action requires some method for turning the gene on or off at the appropriate time. One way in which this is done is by modifying the DNA by adding or removing a methyl group (CH3) to cytosine nucleotides. Addition of the methyl group is thought to turn the gene off, while its removal activates the gene. When the DNA is copied during cell reproduction, the methylation state is also normally copied. Thus a gene that is active (or inactive) in a parent cell may also be active (or inactive) in the daughter cell. If the cell is a reproductive cell, the offspring may inherit the gene activation state of its parent.
    The idea that acquired characteristics can be inherited was popularized by Lamarck in the early 19th century. However, the idea was rejected when the principles of genetics were discovered. Now it appears that there might be some cases in which environmental influences might affect heredity. Some genes respond to environmental conditions, resulting in addition or removal of methyl groups from the DNA. The resulting change in gene activity may appear to be a mutation, although it is actually only a change in gene activation state. Because the state of DNA methylation can be inherited, the change in gene activity may also be inherited. Thus, an environmentally stimulated genetic change can be inherited. This process has been called "epimutation." Epimutations are thought to be more common than changes in DNA sequences. This phenomenon can make it difficult to be certain whether an observed genetic change is due to a mutation or an epimutation. It also suggests that some acquired characteristics may be inherited, although not in the way proposed by Lamarck.

GEOLOGY

Hanson, Bernold M. 1993. What happened to science? American Association of Petroleum Geologists Bulletin 77:1573.

    Quote from the abstract: "Basic mineralogy would have told us that 95% of asbestos fibers are harmless and would have saved taxpayers millions of dollars in the so-called cleanup.... release of chlorine from the sea and volcanoes dwarfs the chlorine released by CFCs.... harmful radiation is not increasing.... air polluting materials produced by man since the beginning of the industrial revolution do not begin to equal the quantities of, toxic materials, aerosols, and particulates spewed into the atmosphere by the volcanoes.... sundry animals and insects also contribute huge amounts of carbon dioxide.... no evidence of widespread forest damage from current levels of acidic rains in the US.... acidity of the soil, not precipitation, determines the acidity in watersheds." Hanson's abstract expresses concern over government regulation based on premature scientific conclusions.

PALEONTOLOGY

Greben, Rebecca and Martin G. Lockley 1993. The Mesozoic and Cenozoic bird track record. a bus in favor of shorebirds Journal of Vertebrate Paleontology (Supplement Abstract) 13:38-39A.

    There are approximately 100 bird trackways known worldwide. About half of those sites are found in Cretaceous deposits, and the other half occur in Cenozoic rocks. Less than 10% of the trackways contains impressions of webbed feet with some occurring in Cretaceous deposits. Duck-like tracks in Eocene through Pliocene rocks also have "dabble marks" (feeding traces). The waterfowl trackways occur in deposits that have been interpreted as shorelines or lake sediments. [Trackway preservation requires rapid sedimentation and cementation. Ed.] The tracksite record is strongly biased in favor of shorebirds and waterfowl. Trackways for grounddwelling birds, perching birds and birds of prey (raptors) are in some cases non-existent.

Hunt, Robert M., Jr., R. I. Skolnick and E. Stepleton. 1993. Denning behavior of large mammalian carnivorans. Oldest burruws found in the earliest Miocene (22 Ma) of North America. Journal of Vertebrate Paleontology (Supplement Abstract) 13:42-43A.

    Two sites in northwest Nebraska have been interpreted as den complexes. The filled burrows contained bones. The site at Beardog Hill (Miocene) contained 2 species of amphicyonid (an extinct dog-like animal the size of a bear with a long, massive tail; short, powerful limbs; spreading, five-toed feet; and tooth structure indicating they were omnivores), 2 species of mustelid (weasel), a small, unspecified canid (dog-like), plus probable prey: juvenile oreodont (pig-like appearance with ruminant or "cud-chewing" tooth structure) and rhinoceros. From the site near Agate National Monument, bones of a wolf-sized amphicyonid, an unspecified rodent and a small fox-like carnivoran have been found in burrows. Den sites are difficult to establish in the fossil record.

DINO NOTES

Carpenter, K. and B. Small. 1993. New evidence for plate arrangement in Stegosaurus steno (Dinosauria). journal of Vertebrate Paleontology, Abstracts 13(3):28A.

    Researchers report the second "road-kill" specimen of a stegosaur has been found about 1.25 km from where the first specimen that was found in 1886. Nearly all the plates along the back were found in place, and the plate arrangement was alternating rather than formed in double rows. The plates along the back may have restricted movement. The neck and end of the tail section had the greatest degree of movement.

Larson, P. L. 1993. Sexual dimorphism in dinosaurs and their relatives. Journal of Vertebrate Paleontology, Abstracts 13(3):46A. Also see: Fischman, J. 1993. To sex a T. rex. Science 262:846.

    Larson compared the tail structures of 14 T. rex specimens to crocodiles, ratites and ducks. The first chevron under the tail of the female crocodile is farther away from the pelvis and smaller in size than that of the male. Similar features were found on the T. rex skeletons. An overall comparison of skeleton size revealed that the 'males' are consistently smaller than the 'females.' According to Sankar Chatterjee (Texas Tech University), "In many modern reptiles, and in birds of prey, the female is larger than the male."

 

GRI NEWS

    Drs. Ben Clausen and Clyde Webster traveled to our Seventh-day Adventist seminaries in Europe for 5 weeks in November and December, 1993. This is the first time GRI staff members have lectured at any of the seminaries in East Europe other than Friedensau. Adalbert Orban, Principal of the Romanian Theological Seminary in Bucharest, described their coming "as refreshing as cool water in a hot desert." Dr. Webster characterized the general level of scientific background of the faculty and students as high, with comments and questions that were insightful and meaningful. The men enjoyed a firsthand geography lesson when they spent a week in Prague (capital of the Czech Republic) and the weekend in Bratislava (capital of Slovakia). In Bratislava they met with SDA students and other university students from the area, as well as some non-SDA professors. After the meeting, these professors gave their business cards to the presiding elder and asked to be contacted if GRI ever returned to their country. We are encouraged by their desire to continue dialogue on the creation issue.
    In late November Dr. Jim Gibson traveled to Helderberg College in South Africa for a Faith and Learning Seminar. He gave four lectures on the interface between creation, science, biology and the Christian faith.
    In early December Dr. Elaine Kennedy gave two workshops at the Annual Ministerial Conference at Oakwood College. The pastors have been concerned about the impact of evolutionary theories taught to their youth attending public schools.

 

PALEOBIOLOGY OF DINOSAURS
M. Elaine Kennedy, Geoscience Research Institute

    "Her first thought was that the dinosaur was extraordinarily beautiful. Books portrayed them as oversize, dumpy creatures, but this long-necked animal had a gracefulness, almost a dignity, about its movements. And it was quick — there was nothing lumbering or dull in its behavior. The sauropod peered alertly at them, and made a low trumpeting sound rather like an elephant."1
   
In recent years paleontologists have witnessed a revolution in their interpretations of the paleobiology of dinosaurs. The fossil record has provided new insight into possible dinosaur behaviors. These interpretations are based on a variety of data.
    The data can be loosely grouped into 7 categories: 1) Bones: fragments, isolated bones, and articulated skeletons; 2) Skulls and teeth; 3) Skin impressions, scales, scutes and spines; 4) Stomach contents, dung, and gastroliths; 5) Eggs, embryos, nests, hatchlings, juveniles; 6) Trackways; 7) Death assemblages: Much information can be gathered from the fossil material and from the entombing sediments.
    Behavioral implications are then postulated based on the data collected. For example, an examination of the Hypsilophodon tail reveals bony structures that restricted tail movement and caused the tail to remain rigid. It has been suggested that the stiff tail was used to maintain balance or as a "dynamic stabilizer" enabling the dinosaur to make sudden turns while evading a predator.2 Areas of muscle attachment on the bones aid in the reconstruction of the animals and provide rough estimates of probable strength and body mass.
    Several behavioral interpretations have been based on the skulls of dinosaurs. The ratio of the cranial capacity to body size is used to estimate intelligence. The ratios are compared to various reptiles, mammals and birds.3 Using this method, it has been postulated that velociraptors had the intelligence of a chicken. In addition to the information available in regard to size and position of ears, eyes and nose on a skull, endocranial casts are examined to determine the sensory abilities.4 The teeth and jaws of the skull provide information about possible diet. For herbivores, associated plant material is also considered (although evidence of an adequate food supply for the very large herbivores is lacking.)5 Additional data that may contribute to our understanding of the dietary habits of dinosaurs would include "petrified stomach contents," gastroliths or gizzard stones and dung. Unfortunately, such materials are difficult to identify accurately. Recent research6 on some isolated clumps in the Two Medicine Formation in Montana, USA, has reported probable dinosaur dung. The deposits consist of conifer xylem that has been burrowed by dung beetles. The coprolites were located near hadrosaur bones and nests.
    Skin impressions have been ascribed to 48 genera.7 Several hadrosaur skin impressions have been found, and careful examination of these skin impressions suggests that the neck was thicker and more muscular than the gooseneck previously proposed for the hadrosaur. In addition, the ruffled frill is probably skin from the side of the neck rather than dermal spines typical of true frills (bony neck protection).8
   
Dinosaur eggs have been known from Mongolia since 1922. The most complete information regarding dinosaur eggs and nests has come from the excavations in Montana, USA. CAT scans have been used to identify dinosaur embryos in eggs. Eggs have been found that contained babies only partially hatched. Bowl-shaped depressions have been found with eggs arranged point down in a spiral pattern. Juveniles with worn teeth have been found in nests with broken eggshell. Several varieties of dinosaur eggs and nests have been discovered. From the database for the maiasaur nesting sites in Montana, it has been postulated that 1) as many as 40 adults laid eggs at the same time and at the same site, 2) the young remained at the nest site and 3) adults stayed in the area to care for the young, behavior that is typical of warmblooded animals.9
    Trackways are used to interpret gait, speed, paleoecology and habitats of dinosaurs. Spacing and arrangement of the tracks determines gait. Theoretically, the quadrupeds and large bipeds preferred walking. Some trackways of smaller bipeds have been interpreted as running or hopping tracks. Parallel tracks are interpreted as herding behavior and migration.10 Such an interpretation assumes that the trackways represent normal behavior. Stress introduced by some catastrophic event would produce a very different interpretation for the tracksites. Trackways are found in a wide variety of deposits. The deposits have been interpreted as a wide variety of paleoenvironments: flood plains; streams, soils, and playa lakes in and regions; deltas and coastal plains.11 The identity of the dinosaurs responsible for the tracks is difficult to ascertain. Track size may vary, and the interpretation of the tracks as those of an adult or juvenile may be unreliable.12
   
Important information is also gathered from death assemblages. When researchers are looking at an extensive deposit of maiasaur bones,13 a velociraptor gripping the head of a protoceratops or an articulated skeleton with contorted neck and tail bones,14 the bone condition and sediments in which the bones were deposited are studied to determine the mode of death, burial and subsequent preservation processes.
    Multiple lines of evidence have been used to address the possibility that dinosaurs may have been warm-blooded. Their large chest cavities and "migratory" behavior have been cited as evidence for endothermic systems.15 Additional evidence for warm-bloodedness comes from research by Barrick and Showers.16 They compared oxygen isotope ratios from the bones of seven dinosaur species to the ratios in bones of a deer, cow and the cold-blooded Komodo dragon. The tail of the Komodo dragon ranged from 4°- 16° colder than its ribs; whereas the mammals had less than 7° difference between the legs and ribs. According to Barrick and Showers the dinosaur ratios fell within the mammal range.
    Despite the broad range of data available, there is much to be learned about dinosaurs and their behavior. Paleobiological interpretations will change as new discoveries are made. It is important to remember that many of the questions that need to be addressed from the perspective of those who accept a biblical explanation for earth's history are not being asked by the secular geologic community.

Endnotes

  1. Crichton, M. 1990. Jurassic Park. Ballantine Books, New York. 399 pp. Paragraph reprinted by permission.
  2. Norman, D. B. 1989. Ornithopod dinosaurs: relationships, structure, and habits. In Padian and Chure (eds), The Age of Dinosaurs, Short Course #2, pp. 58-70. Paleontology Society Publ.
  3. Rowe, T. 1989. The early history of theropods. In Pathan and Chure (eds.), The Age of Dinosaurs, Short Course #2, pp. 100-112. Paleontology Society Publ.
  4. Ibid.
  5. Weishampel, D. B. and D. B. Norman. 1989. Vertebrate herbivory in the Mesozoic: jaws, plants, and evolutionary metrics. In Farlow (ed.), Paleobiology of Dinosaurs. Geological Society of America, Special Paper 238:87-100.
  6. Chin, K. 1993. Evidence for dinosaur/insect interactions in the Cretaceous (Campanian) Two Medicine Formation of Montana. Journal of Vertebrate Paleontology, Abstracts 13(3):29A.
  7. Lambert, D., et al. 1990. The Dinosaur Data Book. Avon Books, New York, pp. 38-105.
  8. Czerkas, S. A. 1993. Frills and goosenecks. Journal of Vertebrate Paleontology, Abstracts 13(3):32A.
  9. Homer, J. R. and J. Gorman. 1988. Digging Dinosaurs. Workman Publishing, New York. 210 pp.
  10. Carpenter, K. 1992. Behavior of hadrosaurs as interpreted from footprints in the "Mesaverde" Group (Campanian) of CO, UT, and WY. Contributions to Geology, University of Wyoming 29:81-96.
  11. Gillette, D. D. and M. G. Lockley (eds.). 1989. Dinosaur Tracks and Traces. Cambridge University Press, New York. 454 pp.
  12. Irby, G. V. 1993. Tracks and trackmakers at a mass dinosaur tracksite, lower Jurassic Dinosaur Canyon Member, Moenave Formation, NE AZ. Journal of Vertebrate Paleontology, Abstracts 13(3):43A.
  13. Homer and Gorman, pp. 128-138.
  14. Lambert, p. 217.
  15. Lemonick, M. D. 1993. Rewriting the book on dinosaurs. Time, April 26, pp. 42-49.
  16. Folger, T. 1993. The blood of dinos. Discover, January, p. 49. See also: Barrick, R. E. and W. J. Showers.

GEOSCIENCE REPORTS
Winter 1994 No.17

Editor - M. Elaine Kennedy
Associate Editor - Katherine Ching

Subscription requests, correspondence, and notices of change of address should be sent to: Geoscience Reports, Geoscience Research Institute, Loma Linda University, Loma Linda, CA 92350 USA Annual subscription rate is $3.00 (U.S. currency).

Geoscience Reports is a newsletter published by the Geoscience Research Institute to present current happenings at the Institute as well as general-interest articles that deal with creation/evolution issues for elementary/secondary-school and college science classes. The views expressed are those of the authors and not necessarily those of the Institute.

Staff of the Institute: Ariel A. Roth, Director (Ph.D., zoology); Ben L. Clausen (Ph.D., nuclear physics); L. Jim Gibson (Ph.D., biology); M. Elaine Kennedy (Ph.D., geology); Clyde L. Webster, (Ph.D., chemistry); Katherine Ching, Editor (M.A., history); and Janet Williams, Administrative Secretary.


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