Apalachee Bay, and the Aucilla River sinkhole at Page-Ladson
Florida drowned sites
People and a mastodon about 14,550 years ago (a sinkhole now under the river, and sites on the Gulf shelf)
Under the Aucilla, a biface lay in sediments dated to about 14,550 calendar years ago, next to a mastodon tusk scored as it was pulled from the skull. Offshore, in a few metres of the Gulf, nine more sites follow the river the sea buried.
Why this is extraordinary
Page-Ladson is a sinkhole in the bed of the Aucilla River, about 11.5 kilometres inland from the Gulf of Mexico, under about 9 metres of water. The sink is about 60 metres across, cut into limestone, and it was not always a river. Around 14,550 calendar years ago it was a pond in the open air. A 2016 study in Science Advances, led by Jessi Halligan and Michael Waters, reports six stone artefacts of local coastal-plain chert in undisturbed sediments there, including a biface, a reworked knife, found in place. Seven radiocarbon samples from immediately beside that biface date to about 14,550 calendar years ago. The piece sat under 1.1 metres of later sediment and under a shell-rich bed dated to about 14,400. A vertical series of 24 radiocarbon samples, from above the biface to below it, falls in order. Seventy-one radiocarbon ages underpin the paper. The sea, rising at the end of the ice age, eventually pushed water and about 4 metres of sediment over the pond and left the site submerged.
A mastodon was already there. In 1993 a tusk came out of the same unit, with multiple parallel grooves across the end that had sat in the skull. The 2016 team looked again and agreed the grooves were made by people, most likely while the tusk was being pulled from its socket. They did not find cut marks on the other bones. Their sentence is that people butchered or scavenged a mastodon beside the pond. Sporormiella, a fungus that grows on dung, and the other proxies in the mud, are their case that hunters and megafauna shared this coast for about 2,000 years, until the animals drop out of the record around 12,600 calendar years ago. A university account of the project places Clovis, the fluted-point horizon long treated as the first widespread culture south of the ice, nearer 13,000 years ago. Page-Ladson is older than that placement on the 2016 clock. The site carries the name of Buddy Page, the diver who brought the sinkhole to archaeologists, and of the Ladson family, who owned the land, which is the University of Michigan’s account of how the place entered the literature.
The shelf is the other half, and it is why the pin sits in the Gulf rather than on the bridge at Lamont. At the last glacial maximum the western Florida shelf reached 185 kilometres or more beyond the modern Aucilla, at depths somewhere between 60 and 100 metres, in Michael Faught’s 2004 report. The Aucilla of that time, the PaleoAucilla, ran across a forested plain that is now Apalachee Bay. Faught’s own work followed one drowned reach of that river. Nine prehistoric sites lie 6 to 9 kilometres off the modern coast, in 4 to 6 metres of seawater, with bifaces and unifaces of late Paleoindian and early Archaic age, and later Middle Archaic material, plus terrestrial animal bone and tree stumps still in place. J&J Hunt is the most dug of them. The tools include a Suwannee point and Bolen points, types of the late Paleoindian and the early Holocene. The edges are sharp. A black stain helps a diver see them. This is not the 14,550-year pond. It is the next country out, drowned later, and it is already yielding camps.
Two other American clocks sit on land that did not drown. Paisley Caves has dated human coprolites. Meadowcroft has early hearths. Far to the north, Bluefish Caves is the Yukon argument. Page-Ladson does not borrow their dates. It has seventy-one of its own. The catch is the size of the toolkit and the size of the shelf. Six artefacts and one grooved tusk are a real association, and they are a small one. The outer shelf, 60 to 100 metres down and 185 kilometres out, is where a glacial coastline would be, and Faught’s nine sites are still in the shallows.
Why it matters
If the 14,550-year surface is secure, people were on the Gulf coastal plain before Clovis, beside animals that still had 2,000 years to live. If the early record is mostly on the shelf, even that sinkhole is the inland edge of a country archaeologists have only started to dive.
The pin is Apalachee Bay, over the drowned lower Aucilla. Page-Ladson itself is 11.5 kilometres inland, under the modern river, and it is part of this room because the same rising sea that covered the shelf also covered the sink. The photograph is the river at a highway bridge, not the dive. The wing is Drowned Lands.
Photo tour
1 photograph, unedited. On a phone, swipe the row. Choose one to look closely.
- No openly licensed photograph of the Page-Ladson sinkhole, or of the biface in place, was found. The river picture is a highway bridge upstream of the site.
What is still unexplained
These sit beside the consensus account, with the same visual weight. None of them is marked solved.
Location and dating
- Location
- The pin is in Apalachee Bay, about 29.7 degrees north and 84.2 degrees west, over the drowned lower course of the Aucilla. Page-Ladson is about 11.5 kilometres inland from the Gulf, under about 9 metres of river, in a sinkhole about 60 metres across. Faught’s nine offshore sites are 6 to 9 kilometres out, in 4 to 6 metres of water, along one reach of the PaleoAucilla. The inland sink and the offshore camps are one river. The pin is the sea, because that is where the glacial plain went.
- Period label
- Current consensus — open to revision Page-Ladson’s occupation surface is about 14,550 calendar years ago, with megafauna in the regional record until about 12,600. The offshore sites run from late Paleoindian types through the early and middle Archaic, which is the early and middle Holocene, the centuries when this part of the shelf was drowning. The glacial coastline, 185 kilometres out, is older than those shallow sites and is almost untested.
- How this dating was done
- Page-Ladson is radiocarbon on organic material in a vertical sequence, seventy-one ages, read against stratigraphy that includes an unbroken shell bed. The tusk grooves are a trace study, a reading of marks. The offshore sites use artefact typology, Suwannee and Bolen and later points, plus the depth of the sea as a latest possible date for life in the air, the same logic as a minimum age. No archaeoastronomy is in either paper.
- What could change it
- A cut mark on a mastodon bone, in the same level as the biface, would thicken the butchery reading the tusk only sketches. A date that broke the vertical order would reopen the question of mixing. On the shelf, a site near the 60-to-100-metre contour, with artefacts in place, would reach the glacial shore the shallow camps do not.
What is actually there
- Page-Ladson, about 9 metres of water, about 11.5 kilometres inland, a sinkhole about 60 metres across.
- Six chert artefacts, one biface in place, seventy-one radiocarbon ages, about 14,550 calendar years ago.
- A 1993 mastodon tusk with parallel grooves, reread in 2016 as human, likely from pulling the tusk free.
- About 2,000 years of overlap with megafauna, which leave the record around 12,600 calendar years ago.
- Nine offshore sites, 6 to 9 kilometres out, in 4 to 6 metres of water, with in-place tree stumps.
- At the glacial maximum the western shelf extended 185 kilometres or more, at 60 to 100 metres depth.
Open questions
| Question | Status |
|---|---|
| Did the biface and the tusk share one afternoon at the pond? | Open. They share a geological unit and a date. A cut mark on the bones would tie the carcass to the tools more tightly than the tusk grooves alone. |
| How much of the early Gulf coast is still on the outer shelf? | Open. The shallow sites are real. The 185-kilometre glacial shore is reconstructed, not excavated. |
The current narrative
Where publication stands today. It is the best-supported reading, and it is open to revision. It is not a verdict.
The current narrative — open to revision
People on the Gulf plain before Clovis
By about 14,550 calendar years ago people at Page-Ladson were using a pond in a sinkhole, and handling a mastodon tusk, on a coastal plain that the rising sea later drowned. The shallow offshore sites continue that drowned landscape into the early Holocene.
What supports this
- Seventy-one radiocarbon ages and an in-place biface under a shell bed.
- Grooves on the tusk, reread as human.
- Nine offshore sites with land animals, tree stumps, and early point types, in a few metres of seawater.
What pushes back
- Six artefacts is a small industry, and old wood or old dung can date a layer older than a visit if the association slips.
- No spear-cut bone was found in the new dig. Scavenging a tusk is a narrower act than a hunt.
- The outer shelf, where the glacial coast was, is not part of the excavated sample.
What would settle it
The association at Page-Ladson is what the dates and the shell bed are for. It would weaken if the vertical sequence were shown to be mixed, and it would widen if the outer shelf produced a site as careful as this one.
Emerging narratives
Other published readings. Each may be right. None is adopted here unless the evidence carries it.
An emerging narrative
The earliest Gulf coast is still underwater
Page-Ladson is the inland pond of a coastal country whose main early camps stood on a shelf that is now the Gulf, much of it still unsurveyed below 40 metres.
What supports this
- Faught’s reconstruction puts the glacial shore 185 kilometres out, at 60 to 100 metres down.
- People were already in the region at 14,550 calendar years ago, when that shore was far to the west of the modern beach.
- The nine shallow sites show that camps survive inundation on this coast.
What pushes back
- Those nine sites are late Paleoindian and Archaic, not dated to 14,550.
- A reconstruction from bathymetry is not a village.
- An inland sinkhole with a secure date does not require the outer shelf to have been the centre.
What would settle it
The reading is a map of the missing country. It becomes a find when someone works the deep contour the way Halligan and Waters worked the sink.
Should the current view be reevaluated?
Open to revision
The 2016 association at Page-Ladson is a strong published case for people on this plain before Clovis. How much of that plain’s early life is under the Gulf, and whether the tusk was a hunt, stay open.
What drives this
- An in-place biface inside a long radiocarbon sequence.
- A shelf whose glacial shoreline has been drawn and not dug.
This is the museum’s own weighing of the evidence. It is not a visitor vote, and it is separate from the slider.
Weigh it yourself
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If the contested reading is right
What would follow if a reading that is not the consensus turned out to be true, and what could settle it. This explains the stakes. It does not adopt the reading.
The main early camps of this coast lie on the outer shelf.
Page-Ladson would be a backwater pond of a drowned coastal society, and the Clovis-first map of the Southeast would have been drawn on the high ground the sea left behind.
Why it is still worth a test
Extend the PaleoAucilla survey from the 4-to-6-metre sites toward the 40-metre and 60-metre contours.
Sources
- Pre-Clovis occupation 14,550 years ago at the Page-Ladson site, Florida Science Advances
- The Underwater Archaeology of Paleolandscapes, Apalachee Bay, Florida American Antiquity
- New evidence that humans settled in southeastern US far earlier than previously believed University of Michigan
Image credits
- The Aucilla River at the US 19 bridge near Lamont, the county line between Jefferson and Madison. Page-Ladson is farther downstream, in a sinkhole under about 9 metres of river. This frame is the river, not the site.. Ebyabe, CC BY-SA 3.0. Shown unedited.