Lucas Family

The TerraMar Collection

Three billion years of the Earth's story, in one house. Every object placed in time, and on the map. The line near the bottom, in gold, is us.

Rock and mineral Shelled animals Life in water Life on land Us Age not pinned down
Press "Real time."

That is what these ages look like when every year gets equal width. Everything after the tiger iron collapses against the right-hand edge, and four hundred million years of animals becomes a single mark. "Stretched" divides by ten at each step so the recent past can be told apart. Nothing else changes.

The jaw and the ammonite nearly met.

The Megalosaurus lived about 167 million years ago. The big cut ammonite is a perisphinctid, roughly 160. Seven million years apart, which at this scale is almost nothing. And the rock the jaw came out of is dated by ammonites from that same family, because the bones washed off the land into a shallow sea and settled among the shells.

Scale the Earth to one year.

The planet forms at midnight on January 1. The tiger iron forms in early May. The trilobite walks a seafloor on November 20. Megalosaurus dies on December 18, Stan on December 26. Our species appears at 11:25 in the evening on December 31, and everything anyone has ever written down happens in the last thirty-six seconds.

The saber-tooth is younger than we are.

Every object here is older than the human species except one. Smilodon went into the tar around twenty-five thousand years ago, by which time people had been on Earth for more than a quarter of a million. Somebody watched that animal die.

Where the Earth gave them up

Seven countries on five continents. TerraMar means land and sea, and this is the land part: every place a piece of this collection came out of the ground.

Drag to spin · tap a marker or a name

About this map: modern coastlines are drawn from the Natural Earth dataset. Every marker is placed from the specimen’s own documented locality, verified against published records.
Tap a marker or a name. Each entry carries its TerraMar number, its species, and where the Earth gave it up.

The worlds they lived in

The continents have not always been where they are. Seven Earths, drawn from our best reconstructions, with the pieces of this collection placed in the world that made them.

Scientific note: these seven Earths are stylized reconstructions, drawn by hand from published paleogeographic research and simplified for clarity. Positions before about 540 million years ago are not reliably known and are shown schematically. These reconstructions reflect the science as of 2026; they are revised when it changes.

Sea, before oxygen — iron-green water Sea — rusted clean, blue ever since Land, bare rock — before plants Land, alive — after plants come ashore

The registry

Every object in the collection, in accession order. Tap an entry for the full record: what the object is, where it came from, what the animal was, who it knew, and how its age is known. The blue links walk the food web. The colored chips name shared worlds: groups that lived in the same place at the same time. Accession codes read collection, year, sequence: TMC-24-001 is the first piece of 2024. Entries marked cast are documented reproductions, here because the originals cannot be owned at any price.

Glossary

The words the labels are written in. Not a dictionary, but a way in: each term here is something the registry above actually uses, explained the way a museum wall would explain it.

Accession number
The permanent identity a museum gives an object when it enters the collection. Once assigned, it never changes and is never reused, so the object and its records can always find each other. The TMC numbers throughout this archive are accession numbers.
Archosaur
The great reptile lineage that includes crocodilians, pterosaurs, dinosaurs, and birds. Two of its branches are still alive today: every crocodile and every bird you have ever seen.
Biostratigraphy
Dating rock by the fossils inside it. Some species lived briefly and spread widely, so finding one pins the rock to a narrow window of time. Many of the ages in this registry are known this way.
Cambrian Explosion
The burst of animal evolution beginning roughly 538 million years ago, when most of the major animal body plans appear in the fossil record within a few tens of millions of years. Eyes, shells, and legs all date from this interval, which is why the fossil record becomes suddenly rich there.
Carboniferous
The period from about 359 to 299 million years ago, when vast swamp forests covered the continents. The coal that powered the industrial world is those forests, buried and compressed, which is where the period gets its name.
Cast
A three-dimensional copy of a fossil, made by pouring material into a mould taken from the original. A good cast records the exact geometry of the specimen, and casts are how important fossils have been studied and shared between institutions since the 1800s, long before photography or scanning.
Cenomanian
A stage of the Late Cretaceous, roughly 100 to 94 million years ago. The Kem Kem river system, with its sawfish and giant predators, belongs to this window.
Clade
A natural group in the tree of life: an ancestor and every one of its descendants, with nothing left out. Birds and dinosaurs form a clade. "Fish," as commonly used, does not, because it leaves out the land animals that descended from them.
Composite
A specimen assembled from the remains of more than one individual animal. Composites are legitimate in science and in collections when they are disclosed; undisclosed, they are misrepresentation. The difference is entirely in the label.
Conservation
The care that keeps an object stable over time: controlling humidity and light, stabilizing cracks, and documenting every intervention so future caretakers know what was done and why.
Deep time
Time at geological scale, measured in millions and billions of years rather than centuries. Human intuition fails at this scale, which is why the timeline at the top of this page offers two ways of drawing it.
Dinosaur
A member of Dinosauria, the group named by Richard Owen in 1842. Dinosaurs are a specific branch of reptiles defined by their anatomy, especially an upright stance. Marine reptiles like mosasaurs and plesiosaurs are not dinosaurs, and one branch of dinosaurs, the birds, is still here.
Epoch
A subdivision of a period. The Pleistocene, when Smilodon hunted in California, is an epoch of the current period, the Quaternary.
Era
One of the largest divisions of Earth's history. The colored bands on the timeline are eras: Archean, Proterozoic, Paleozoic, Mesozoic, Cenozoic. Each ends at a profound change in the world, usually a mass extinction.
Extinction
The end of a species: the death of its last individual. It is the fate of almost every species that has ever existed. More than ninety-nine percent of everything that has ever lived is extinct.
Formation
A named, mappable body of rock with a consistent character, the basic unit geologists use to organize the Earth's crust. Hell Creek, Kem Kem, and Cleaverville are formations. Naming the formation is how a fossil's origin becomes checkable rather than a story.
Fossilization
Any of the processes that preserve evidence of ancient life in rock. It is rare: the overwhelming majority of organisms decay without a trace. Everything in this registry is an exception to that rule.
Genus
The rank above species, grouping the closest relatives together, and the first word in a scientific name. In Tyrannosaurus rex, the genus is Tyrannosaurus. A genus can hold one species or many.
Geological age
How old a rock or fossil is, expressed either in years (numerical age, usually from radiometric dating) or by position in the sequence of named intervals (relative age). The registry gives both wherever both are known.
Holotype
The single physical specimen a species' name is permanently anchored to. When Buckland described Megalosaurus in 1824, the Oxford jaw became part of the material that defines the name forever. If questions arise about what a species is, science returns to the type material.
Horizon
A specific level within a rock formation, often only inches thick. Recording the horizon a fossil came from places it in time far more precisely than the formation alone.
Index fossil
A species so short-lived and widespread that its presence dates the rock it is found in. Ammonites are among the best index fossils ever: the Stonesfield Slate that produced the Megalosaurus jaw is dated by them.
Lectotype
When a species was originally described from several specimens without one being singled out, a lectotype is the specimen later chosen from that original group to carry the name. The Megalosaurus dentary in Oxford became a lectotype this way.
Locality
The specific place a specimen came out of the ground, ideally named to the quarry or site, not just the country. Locality is the difference between "from Morocco" and "from the Ouled Abdoun Basin, near Khouribga." Every marker on the globe above is a locality.
Maastrichtian
The final stage of the Cretaceous, 72 to 66 million years ago, and the last age of the dinosaurs. The Khouribga sea, Hell Creek, and the asteroid all belong to it.
Marine reptile
A reptile that returned to the sea. Mosasaurs, plesiosaurs, and ichthyosaurs each did this independently, from different land-living ancestors, and each solved the same problems of swimming, breathing, and hunting a different way. None of them are dinosaurs.
Mass extinction
A global collapse in which a large fraction of all species dies out in a geologically short time. Five great ones mark the record. The end-Permian was the worst; the end-Cretaceous, 66 million years ago, is the one that ended most of the animals in this room.
Matrix
The rock a fossil is embedded in. Sometimes it is removed in preparation; sometimes it is kept, because the surrounding rock is itself part of the evidence, recording the environment the animal came to rest in.
Member
A named subdivision of a formation, used when a formation contains distinct layers worth telling apart. Formation, member, horizon: each step narrows the address.
Neotype
A replacement type specimen, formally designated when the original type material has been lost or destroyed. It exists so a species' name never floats free of a physical object.
Original material
Actual fossil: bone, tooth, or shell preserved from the animal itself, as opposed to a cast or reconstruction. In this archive, whether an object is original material is always stated plainly.
Ornithischian
One of the great branches of dinosaurs, including Triceratops, the duckbills, and the armored forms. The name means "bird-hipped," which is one of paleontology's small jokes: birds actually descend from the other branch.
Period
The workhorse division of geological time, sitting between era and epoch. Jurassic, Cretaceous, and Ordovician are periods. Most of the ages in this registry are given by period and stage.
Permineralization
A common form of fossilization in which mineral-rich water seeps into the pores of bone or wood and deposits minerals there, turning the tissue to stone while preserving its structure, sometimes down to the cell.
Preparation
The skilled work of freeing a fossil from its matrix and stabilizing it, done with needles, brushes, air tools, and patience. Good preparation can take longer than the excavation, and bad preparation can destroy what millions of years preserved.
Provenance
The documented history of an object: where it came out of the ground, who has held it since, and how it got here. Provenance is what separates a specimen from a curiosity. It is the standard every object in this archive is held to.
Radiometric dating
Measuring the age of rock by the steady decay of radioactive elements inside it, like reading a clock that started when the rock formed. It is how numbers like "66 million years" are known rather than guessed.
Reconstruction
An informed scientific estimate of missing anatomy or of what an animal looked like in life, built from the evidence that survives. Every mounted skeleton and every painting of a living dinosaur is a reconstruction, and good ones change as the science does.
Replica
A copy of a specimen. The best replicas are casts taken from moulds of the original; lesser ones are sculpted approximations. A replica honestly labeled is an educational object. A replica sold as original material is a forgery.
Restoration
Repair or replacement of missing parts of an actual fossil, such as filling cracks or rebuilding a broken edge. Some restoration is normal and accepted; what matters is that its extent is disclosed, so no one mistakes plaster for bone.
Sauropod
The long-necked giant dinosaurs, the largest land animals that have ever existed. Some exceeded a hundred feet and thirty tons, walking on four columnar legs and eating their way through entire landscapes.
Species
The basic unit of biological diversity, written as the second word of a scientific name: the rex in Tyrannosaurus rex. Defining where one fossil species ends and another begins is genuinely hard, and honest labels say so when it is uncertain.
Stratigraphy
The study of rock layers and their order. Its founding insight is simple and powerful: in undisturbed rock, deeper is older. Stratigraphy is how the Earth's history was first put in sequence, before anyone could put numbers on it.
Stylized reconstruction
A reconstruction simplified for clarity rather than drawn to full scientific precision, and labeled as such. The seven ancient Earths above are stylized reconstructions: faithful to the published research, simplified so the shape of the story can be seen.
Synapsid
The lineage that includes mammals and their extinct relatives, distinct from reptiles for over 300 million years. The sail-backed Dimetrodon, often mistaken for a dinosaur, is a synapsid: it is more closely related to you than to any dinosaur that ever lived.
Taxonomy
The science of naming and classifying life. Names are hypotheses, not permanent labels, which is why a tooth sold under one name can honestly be relabeled when the science moves. This registry keeps both names when that happens, because the history of the name is part of the record.
Theropod
The branch of dinosaurs that includes nearly all the meat-eaters: Megalosaurus, Spinosaurus, Carcharodontosaurus, Tyrannosaurus. It is also the branch that survived. Every bird alive today is a theropod dinosaur.
Trace fossil
Preserved evidence of an animal's behavior rather than its body: footprints, burrows, bite marks, nests. A body fossil shows what an animal was; a trace fossil shows what it did.
Type specimen
The physical specimen or specimens that a species' scientific name is formally attached to, held in a public institution so any scientist can examine them. Holotypes, lectotypes, and neotypes are all kinds of type specimen. They are the anchors of the entire naming system.

About TerraMar

A collection born from a child's wonder, built to preserve three billion years of Earth's story alongside one family's own.

TerraMar began with my daughter, Nova.

Like many children, she fell in love with dinosaurs. But over time I realized it wasn't simply a childhood fascination. She saw them with a sense of wonder that was impossible to ignore. As her father, I found myself drawn into that same curiosity. One fossil became another, then another, and before long we weren't simply collecting prehistoric objects—we were learning the story of our planet together.

Along the way I discovered something else. My wife shared that same fascination, though I hadn't fully appreciated it when we first met. As a family, we found ourselves spending weekends visiting natural history museums, exploring prehistoric life, and asking bigger questions about where we came from and how our world came to be. Now all three of our daughters also share a similar sense of wonder.

Looking back, that path makes perfect sense.

Long before TerraMar existed, I felt most at home outdoors. I grew up hiking, camping, exploring caves, climbing mountains, rappelling, whitewater rafting, hunting, fishing, and eventually scuba diving. My parents raised my brother and me with a deep appreciation for the natural world, encouraging us to experience it firsthand rather than simply observe it. Photography came much later—not as the beginning of that journey, but as a way to preserve and share the places, wildlife, landscapes, and moments that had already shaped my life. Looking back, TerraMar feels like a natural continuation of that same path. Prehistoric life—dinosaurs, ancient marine reptiles, fossils, minerals, and the deep history of our planet—simply became another way of exploring the world with the same sense of curiosity and wonder that first drew me outdoors as a child.

As the collection grew, I noticed something that surprised me.

Too often, collections become invisible. A fossil is purchased, placed on a shelf, and eventually forgotten. Its story disappears long before the object does.

I wanted something different.

I wanted a place where every specimen could be understood, where every object had a reason for being here, and where my children could one day discover not only what we collected, but why we chose to preserve it.

That idea became TerraMar.

What began as a simple registry slowly evolved into something much larger: a living archive of Earth's history intertwined with our own family's journey. Every entry documents more than an object. It captures a place, a moment in deep time, the evidence behind it, and often the personal story that brought it into our home.

One realization changed the way I looked at the entire collection.

When I arranged everything chronologically, I discovered that our home contained more than three billion years of Earth's history.

Holding that span of time in your hands is difficult to comprehend. It transforms a shelf of fossils into a timeline of life itself.

TerraMar was designed with longevity in mind. It is intentionally simple, built on open web technologies that can be preserved, moved, and maintained for decades to come. My hope is that whether someone opens these pages next year or fifty years from now, they will still be able to explore this collection and understand the stories it preserves.

I don't know what TerraMar will look like in the future.

Perhaps my daughters will add to it.

Perhaps it will remain exactly as it is today.

Either outcome is perfectly fine.

Because TerraMar was never built simply to collect fossils.

It was built to preserve curiosity.

To encourage questions.

To celebrate discovery.

And to remind our family that the greatest stories on Earth began long before we did—and will continue long after us.

Lucas Family · TerraMar Collection · 2024–2026