Chapter 6: Fossil Preservation

Daniel Hauptvogel; Virginia Sisson

Chapter 6: Fossil Preservation

Daniel Hauptvogel and Virginia Sisson

Learning Objectives

The goals of this chapter are to:

Explain the different ways organisms become fossilized
Identify the mode of preservation for fossils

6.1 Introduction

Everyone has heard the word fossil! So, how do you define this term? In this lab, we will define it to mean any evidence for the existence of prehistoric life. What is difficult to explain in this definition is what is meant by prehistoric. For example, would you consider bodies preserved at Pompeii to be fossils, or how about the remains of a frozen mastodon from the Pleistocene that was preserved well enough to be eaten? Some say anything older than 11,000 years is a fossil, but this part of our definition is a matter of semantics. An excellent place to learn more about fossils and fossilization is the Digital Atlas of Ancient Life.

Exercise 6.1 – Fossilization Probability

We start this chapter on how organisms become fossilized with a quick exercise. Figure 6.1 contains three different organisms.

Three images of living organisms; from left to right these show several worms in soil, giant kelp, and mussel shells. — Figure 6.1 – a) Worms, b) Giant kelp; c) Mussel shells. Image credit: a) Soil-Net, CC BY-NC-SA; b) NPS, Public Domain; c) Linnaea Mallette, Public Domain.

Which organism in Figure 6.1 do you think has the highest chance to become a fossil and why?
Which organism do you think has the highest chance to leave behind a trace fossil? ____________________

6.2 Types of Preservation

Taphonomy is the branch of paleontology that focuses on the fossilization process. Fossils are preserved by three main methods: unaltered soft or hard parts, altered hard parts, and trace fossils. You already learned about trace fossils in Chapter 4.

Unaltered fossils are rare except as captured in amber, trapped in tar, dried out, or frozen as a preserved wooly mammoth. Amber is the fossilized tree resin that can trap flowers, worms, insects, and small amphibians and mammals. The father of one of the authors was part of a gold mining operation that discovered a wooly mammoth calf (nicknamed Effie) in Alaska. This was the first mummified mammoth remains found in North America. Even though it was buried about 21,300 years ago, it still consists of tissue and hair. Sometimes, only organic residue is left behind and is detected by molecular, biochemical techniques. Earth’s oldest fossils are only preserved as complex organic molecules.

Soft tissue is hard to preserve because it needs to be buried before bacterial decay can occur. This preservation occurs when remains are buried rapidly in an oxygen-free, low-energy sedimentary environment. Since these conditions are uncommon, the preservation of soft tissue rarely happens. Instead, typical examples of unaltered fossils are skeletal material that has been preserved with little or no change. Many marine invertebrate fossils and microfossils were preserved in this manner. However, paleontologists are now looking closer at fossils and recognizing thin carbon layers in the rock around fossils as soft tissue. Recently, a team led by Mark Norell, a paleontologist at the American Museum of Natural History in New York City, identified a layer of carbon around dinosaur embryos formed over 200 million years ago that they think was a soft eggshell!

Unaltered fossils contain minerals that were biologically produced; these include apatite (in bones and teeth and rarely in exoskeletons, hardness = 5), calcite (calcium carbonate found in many organisms such as shells, hardness = 3, fizzes in acid), aragonite (similar to calcite, but an unstable polymorph) and opal (a type of silica found in marine animals and plants, hardness = 7). In addition, the hard parts (exoskeleton) of some insects and arthropods are made of chitin, a polysaccharide related to cellulose. If you can identify the minerals present in a fossil, you can distinguish if it is original material or altered.

Alteration of hard parts is much more common in fossils and happens when original skeletal material is either permineralized, recrystallized, replaced, carbonized, or dissolved (Table 6.1).

Table 6.1 – Common types of fossil preservation
Type of Preservation	Example
Permineralization occurs in porous tissue such as bone and wood. In this type of preservation, minerals dissolved in water such as quartz, calcite, or pyrite permeate the pore space and crystallize. The addition of these minerals results in denser and more durable fossils. The original bone or wood material may be preserved, or it may be replaced or recrystallized.	Figure 6.2 – Petrified wood from the Petrified Forest National Park, AZ. Image credit: Jon Sullivan, Public Domain.
Recrystallization involves a change in the crystal structure but not in mineral chemistry, similar to recrystallization in metamorphic rocks. For example, the mineral aragonite, a common mineral of many shells, sometimes changes to calcite, a more geologically stable form of the same chemical composition, CaCO₃ (aka a polymorph). Typically, the overall size and shape of a recrystallized fossil do not vary substantially from the original unaltered specimen, but fine details may be lost.	Figure 6.3 – Recrystallized, Silurian-age coral from Ohio. Image credit: James St. John, CC BY.
Replacement is the substitution of original skeletal material by a secondary mineral. For example, the calcite of an oyster shell may be replaced on a molecule-by-molecule basis by silica. Remarkably, the replaced fossil may retain some of the fine cellular detail present in the original even though its composition changed. In this type of fossilization, pore space is not filled, and the fossils are not as dense. The most common replacement minerals are silica (quartz), pyrite, dolomite, and hematite. Replacement by pyrite creates some spectacular fossils, especially those hosted by black shales!	Figure 6.4 – Pyritized fossil trilobite with appendages (Triarthrus eatoni) from the Whetstone Gulf Formation, Upper Ordovician; New York State, USA. Image credit: James St. John, CC BY.
Carbonization is a type of fossil preservation in which the organism is preserved as a residual, thin film of carbon instead of the original organic matter. Leaves, fish, and graptolites are commonly preserved in this way. Compression of the original organism results in thin layers of carbon. Carbonization can also result in the formation of coal.	Figure 6.5 – Carbonization of Silurian-aged graptolites from Poland. Image credit: James St. John, CC BY.
Molds and casts form when the original skeletal material dissolves. The organism leaves behind an impression in the sediment called a mold. If that impression fills with new sediment, it creates a cast. Thus, casts are made from molds.	Figure 6.6 – A mold (left) and cast (right) of a trilobite fossil. Image credit: Roger Wellner.
Internal molds form when sediment fills the inside of a shell before it dissolves; this occurs inside bivalves, snails, or skulls. Often, people confuse casts and internal molds because both have positive relief. However, internal molds preserve a 3-dimensional mold of the inside of the organism, whereas a cast preserves the structure of the outermost part of the organism.	Figure 6.7 – Dissolution of a gastropod that has left an internal mold of the organism. Fossil from eastern Iowa. Image credit: James St. John, CC BY.

Trace fossils, which we discussed in Chapter 4, are not really fossils but the evidence that organisms affected the sediment by burrowing, walking, or even leaving behind excrement or vomit. No kidding, there is fossil poop; this kind of trace fossil is called a “coprolite,” from the Greek word kopros, meaning dung. One last rare type of trace fossil is gastroliths, extremely smooth polished stones that aided digestion in dinosaurs and crocodilia. These are more highly polished than stream-worn gravels. Gastroliths found in Jurassic sediments in Wyoming may have been carried by sauropods over 1600 kilometers from their source in Wisconsin.

Figure 6.8 – Different parts of organisms compared to how they can be preserved as fossils. The green circles are common types of fossilization, the light green, stippled circles are less common, and the light green circles are uncommon to rare ways. Image credit. VB Sisson modified from Ritter and Peterson (2015) CC-BY-SA-NC.

Types of fossilization including alteration, replacement that result in casts and molds. — Figure 6.9 – Types of fossilization including alteration and replacement of the original shell. Follow the arrows from box to box to see how different processes can result in molds and casts. The brown color is a sedimentary rock. The random pattern represents recrystallized carbonate, and the stippled pattern represents secondary minerals such as silica or pyrite. Image credit: VB Sisson with a shell showing growth lines and internal structure adapted from Casella et al., 2017 and fossilization processes adapted from Ritter and Peterson (2015) CC-BY-NC-SA.

3-D Model Box 6.1 – Molds

This model shows a preserved fossil shell on the right (not a cast, original) and an external mold on the left of the ammonoid cephalopod Gunnarites sp. from the Cretaceous Lopez de Bertodano Formation of Snow Hill Island, Antarctica. The fossil specimen is from the collections of the Paleontological Research Institution, Ithaca, New York. The diameter of the specimen (not including surrounding rock) is approximately 9 cm.

Cephalopod: Gunnarites sp. (PRI 61543)
by Digital Atlas of Ancient Life
on Sketchfab

This is an example of an internal (1) and external (2) mold of the gastropod Cassidaria mirabilis from the Cretaceous of Snow Hill Island, Antarctica. The specimen is from the collections of the Paleontological Research Institution, Ithaca, New York. It is approximately 6 cm in length (not including surrounding rock).

Gastropod: Cassidaria mirabilis (PRI 58468)
by Digital Atlas of Ancient Life
on Sketchfab

More 3-D models on fossil preservation can be found at the Digital Atlas of Ancient Life.

If you ever get asked by a friend to help identify a fossil, watch out for pseudofossils, which are accidents of diagenesis that look like a fossil but are just weird sedimentary formations. Pseudofossils include septarian nodules that are mistaken for reptile skin or turtle shells, concretions are mistaken for eggs, and manganese oxide dendrites mistaken for ferns moss.

6.3 Handling of Fossils

Some fossils are incredibly fragile. Some delicate samples are prepared by air abrasion with talcum powder to remove the matrix. For some trilobite specimens, this takes thousands of hours to expose their delicate features. Some fossils you will use may be easy to replace and others impossible. Others may be part of a faculty member’s personal collection. Only handle the specimens that your instructor says you can. If you are taking this lab when teaching is face-to-face in a lab setting, you will handle both real and replica specimens of fossils. While these may have been around for millions or billions of years and seem like they are now rocks, they need to be treated with respect. Some of the fossils that you may handle may be the only specimen of their kind in the collection. Some of the larger specimens may be heavy, especially those that are molds filled with sediment. Never try to scratch the specimens for hardness. Also, never use acid as a mineral test. Finally, if you break or steal a specimen, you will be charged for its replacement.

You are free to make sketches or photograph the specimens. If you do this, you may want to put a scale in the image, such as a coin or ruler. This will help you remember the size of the object. Some specimens will have labels or numbers written on them, and others will not because they may be too fragile to even be written on. You must put each specimen back in its appropriate box or location in a lab tray. Also, do not move any of the paper labels from the boxes. This will prevent confusion for other lab students.

If you’ve wondered how to start your own fossil collection, you can either find them on your own or buy them. The price of fossils for sale ranges from cheap to outrageously expensive. For example, in 2020, an anonymous collector bought a fossil Tyrannosaurus rex, nicknamed Stan, for $31.85 million. This specimen only had 188 bones and was one of the most complete of its species. If this is beyond your budget, you can find inexpensive fossils such as fossilized snails from Morocco for only $0.30 each.

Exercise 6.2 – Identifying Types of Fossil Preservation

Inspect the first set of samples and fill out the table with information about the presence of original biologic material, positive and negative relief, and mineral composition of the samples. Identify the mode of preservation of the fossils. Use the flowchart in Figure 6.10 to help.

Figure 6.10 – Flowchart for identifying the type of fossil preservation. Image credit: Virginia Sisson and Daniel Hauptvogel CC-BY-NC-SA.

Table 6.1 – Worksheet for Exercise 6.2
Sample	Original Material Present?	Relief*	Mineral Composition*	Type of Preservation

*Note that you may not see relief or be able to identify the mineral. Leave these blank if necessary.

Critical Thinking: Which mode of preservation do you think is most common?

Exercise 6.3 – Thinking about Preservation

The way an organism can become fossilized depends on many things. Below are some examples to think about.

Examine an external mold in your fossil collection. These commonly preserve details such as the veins in leaves or scales of fish.
1. What is the grain size of the surrounding rock? ____________________
2. Do you think these impressions could be preserved in coarse-grained sediment?
Look at some examples of carbonization. The dark matter is the remnant of organic carbon that was never oxidized (decayed). Under what conditions might this kind of preservation occur?
Your fossil collection may have graptolites, an extinct planktonic, colonial organism that secreted an organic shell of chitin similar to your cellulose. These colonies are usually preserved as two-dimensional impressions, almost always black (indicating carbonization of the chitin).
1. What type of rocks is best suited to finding graptolites?
2. What were the burial conditions?
Some bones and teeth can be preserved, such as unaltered bones or shark teeth.
1. How would you distinguish these from permineralized fossil bones?
2. Can permineralized wood scratch glass?
Now consider the wide range of sedimentary environments.
1. What sedimentary environments are not suitable for preserving fossils?
2. Which sedimentary environments are good for preserving fossils?
3. How can the energy of the sedimentary environment affect the preservation of fossils?
Critical Thinking: Can volcanic eruptions preserve fossils? Explain.
Critical Thinking: Can you find fossils in metamorphic rocks? If so, what factors aid in their preservation?
Critical Thinking: There are more invertebrates than vertebrate fossils in this lab exercise. Explain why this is.

Exercise 6.4 – Modes of Preservation in an Ancient Reef

During the Permian time, 299 to 252 million years ago, an extensive reef system grew in west Texas at the edge of a small inland marine basin that extended over 26,000 km² (10,000 square miles). Now it is called the Delaware basin, home to a major oil field (Figure 6.11). This reef is now exposed in three mountain ranges; Apache, Guadalupe, and Glass Mountains. Elsewhere, the reef is now buried around the entire rim of the basin. The northernmost exposure of the reef is part of the Guadalupe Mountains National Park. It is home to Carlsbad Caverns, which has the largest underground chamber in the United States. The reef was home to many fossils, including ammonoids, bryozoans, algae, sponges, brachiopods, gastropods, pelecypods, echinoids, fusulinids, trilobites, corals, and crinoids.

Map of exposed Permian reef around the Delaware Basin — Figure 6.11 – Map of exposed and unexposed Permian reef that encircled the Delaware Basin, an inland sea in Texas and New Mexico. Image credit: Adapted by VB Sisson from National Park Service CC-BY-NC-SA.

Unlike modern coral reefs, such as the Great Barrier reef of Australia or the reefs off the coast of Florida and Belize, it was constructed from sponges, algae, and lacy animals called bryozoa. One magnificent exposure of this reef is El Capitan in the Guadalupe Mountains National Park. The reef is subdivided into three parts: back reef, reef, and fore reef. Each had its own unique ecosystem as well as lithology and preservation. The deep part of this basin reached depths of almost 800 meters (½ mile) and is where a lot of organic matter was deposited, leaving black shales – the source of petroleum.

Structure of Devonian reef — Figure 6.12 – Schematic cross-section across a reef showing the back reef, reef, and fore reef as well as the marine basin. Image credit: Adapted by VB Sisson from National Park System CC-BY-NC-SA.

The Delaware inland sea had a narrow outlet to the Panthalassan ocean, much like the Black Sea today. However, after ~30 million years, the entrance got restricted, and the basin started to dry up, forming extensive evaporite deposits (Castille and Salado Formations). This created supersaturated, acidic brines that started to dissolve the underlying carbonate reef, forming extensive caves and karst that you can now visit at Carlsbad Caverns National Park and Lechuguilla Cave, the 8th longest explored cave in the world at ~220 km or 138 miles long. These brines also dissolved the silica-rich sponges that formed the reef and affected the fossil preservation in parts of this Permian reef system.

Google Street View in Google Maps has recorded many of the trails in Guadalupe Mountains National Park. Start at either McKittrick Canyon or the trail to Guadalupe Peak and drag the orange person icon onto one of the trails to see views of the massive limestone reef.

The stratigraphy of this basin is complicated because it varies with time and position in the reef. According to recent sequence stratigraphic analysis, there were up to six transgressive-regressive sequences in this basin (Kerans and Kempter, 2002). Figure 6.13 gives a simplified stratigraphy for the basin during the Permian.

Figure 6.13 – Simplified stratigraphy for the Delaware Basin. Image credit: Simplified by Virginia Sisson from Kerans and Kempter (2002) CC-BY-NC-SA.

Fossils in the Capitan Formation of the Glass Mountains are uniquely preserved (see Figure 6.4). Paleontologists found that it is easy to dissolve away the host carbonate in weak acid and leave behind spectacular specimens.

Figure 6.14 – Fossils from the Capitan Formation of the Glass Mountains, Texas. a) silicified fossils including the wavy outer layer of a bivalve shell and attached to it, are encrusting organisms (sclerobionts). Other fossils include a long tube of a rugose coral with a ribbed athyrid brachiopod at its base; b) silicified Productid brachiopod ventral valve; c) silicified *Hercosestria cribrosa*; d) silicified Anthozoa Brachiopoda, Bryozoa, and rugose coral. Image credits: a) James Wilson, CC0 Public Domain; b) Wikimedia user Wilson44691, CC0 Public Domain; c) Wikimedia user Mark A Wilson Wilson44691, CC0 Public Domain; d) Wikimedia user the paleobear CC BY.

The mineral in these fossils is harder than glass and does not fizz as it is no longer a carbonate. Sometimes this mineral is just a coating, and other times the entire fossil is this new mineral.
1. What is the mineral? ____________________
2. What is the mode of preservation for these fossils? ____________________
3. Were fluids involved in their preservation? If so, what was their composition?
4. Why do you think this type of preservation is found in this one stratigraphic unit.
5. Which part of the reef were these fossils found? Back reef, reef, fore reef or basin? ____________________
  
  Figure 6.15 – Fossilized jaw with teeth of a Helicoprion ferri. The fish associated with this ~35 cm jaw is estimated to be 4 m (~12′) long, but they could reach up to 10 m in length. Also shown are two possible reconstructions envisioned by paleontologists. The first image was common in the 1900s to 1960s. In 2013, CT imaging revealed a different reconstruction. Their primary food source was bottom-dwelling organisms and possibly ammonites. Image credit: Photo is from James St John CC BY 2.0, Reconstructions adapted by VB Sisson from Tapinila et al. 2013 CC-BY-NC-SA.
Elsewhere in the Skinner Ranch Formation of the Glass Mountains, fossils include this amazing saw-toothed whorl of teeth from an extinct shark-like fish known as Helicoprion.
1. Using Figure 6.15, what type of sediment is this fossil found in? ____________________
2. What is this mode of preservation for this fossil? ____________________
3. Where in the reef did Helicoprion live? Back reef, reef, fore reef, or basin? ____________________
  
  Figure 6.16 – Four fossils from El Capitan reef in Guadalupe Mountain National Park. a) Sponge (Porifera), b) Fenestrate bryozoa, c) Polydiexidina fusulinids (foraminifera), d) Fragment of an ammonite. Image credit: a) Jennifer Trout National Park Service public domain; b) Peter Scholle, used with permission; c) Image from Verydeadthings CC; d) Richard Langford UT El Paso, CC.
In the Guadalupe Mountains, you can find thick carbonate layers with many fossils, such as in Figure 6.16:
1. What is the mineral? ____________________
2. What is the mode of preservation for these fossils? Note, there could be more than one mode of preservation. ____________________
3. Were fluids involved in their preservation? If so, what was their composition?
4. Why do you think this type of preservation is found in this portion of the reef?
5. Which part of the reef were these fossils found? Back reef, reef, fore reef or basin? ____________________
Critical Thinking: Summarize your observations about the modes of preservation in different parts of the Permian reef system. Can you explain why the preservation is the same or different around the ancient reef?

Additional Information

Exercise Contributions

Virginia Sisson and Daniel Hauptvogel

References

Casella, L.A., Griesshaber, E., Yin, X., Ziegler, A., Mavromatis, V., Müller, D., Ritter, A.-C., Hippler, D., HarperE.M/, Dietzel, M., Immenhauser, A., Schöne, B.R., Angiolini, L., and Schmahl, W.W., 2017, Biogeosciences, 14, 1461–1492, doi:10.5194/bg-14-1461-2017.

Cooper, G.A., and Grant, R.E., 1964, New Permian stratigraphic units in Glass Mountains, West Texas: American Association of Petroleum Geologists Bulletin 48: 1581-1588.

Cooper, G.A., and Grant, R.E. 1966. Permian rock units in the Glass Mountains, West Texas, In: Contributions to stratigraphy, 1966: U.S. Geological Survey Bulletin 1244-E: E1-E9.

Kerans, C., and Kempter, K., 2002, Hierarchical stratigraphic analysis of a carbonate platform, Permian of the Guadalupe Mountains: The University of Texas at Austin, Bureau of Economic Geology (American Association of Petroleum Geologists/Datapages Discovery Series No. 5), CD-ROM.

Norell, M.A., Weimann, J., Fabbri, M., Yu, C., Marsicano, C.A., Moore-Nall, A., Varricchio, D.J., Pol, D., and Zelinitsky, D.A., 2020, The first dinosaur egg was soft. Nature, 583, 406-410, Published online June 17, 2020. doi: 10.1038/s41586-020-2412-8

Olszewski, T.D. and Erwin, D.H. 2009. Change and stability in Permian brachiopod communities from western Texas. Palaios 24: 27-40.

Ritter, S., and Peterson, M., 2015, Interpreting Earth History: A Manual in Historical Geology, Eighth Edition, Waveland Press Inc., 291 pp.

Scholle, P.A., Goldstein, R.H., and Ulmer-Scholle, D.S., 2007, Classic Upper Paleozoic reefs and bioherms of west Texas and New Mexico: A field guide to the Guadalupe and Sacramento Mountains of west Texas and New Mexico. New Mexico Bureau of Geology and Mineral Resources Open File Report 504, 178 pp.

Tapanila, L., Pruitt, J., Pradel, A., Wilga, C.D., Ramsay, J.D., Schlader, R., and Didier, D.D., 2013, Jaws for a spiral-tooth whorl: CT images reveal novel adaptation and phylogeny in fossil Helicoprion. Biology Letters, 9, 20130057. http://dx.doi.org/10.1098/rsbl.2013.0057

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