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Botuverá Cave, Brazil · one stalagmite · 115,000 years

One drop at a time

Water drips from a cave ceiling onto a stone. Each drop leaves a film too thin to see. Keep it up for 115,000 years and you get about 70 centimetres of stone, with the water’s chemistry kept in every layer.

Botuverá Cave, Brazil

A drop of water

Rain soaks through the soil above a cave and picks up carbon dioxide, which lets the water dissolve a little limestone. When a drop falls in the cave, it loses some of that gas and leaves a thin film of calcite on the stone below.

The stone on screen is a stalagmite called BT-2, from Botuverá Cave in southern Brazil. The database lists its top as still forming, dated to the year 2000.

The top of the stone

A film of stone

Between its top and its first date, which is about 2,300 years old, BT-2 grew about 8.3 millimetres in a thousand years. On average that is less than a hundredth of a millimetre a year. The thin layers at the top are drawn at that spacing; this stone’s yearly layers were not measured.

Further down, each colour is a measurement. Oxygen atoms come in a lighter and a heavier kind, and the stone keeps the mix that was in the dripping water. Blue is lighter, orange heavier.

Eighty years

A lifetime of stone

At that rate, a life of 80 years adds 0.67 millimetres. That is thinner than a credit card (0.76 millimetres).

19 millimetres down

The first date

A layer cannot tell you its age, so scientists measure it. They take small samples and measure how much thorium has built up from the decay of uranium. The first measured date, 19 millimetres down, is 2,245 years, give or take 130 (a 95% range).

Each date is a small mark on the edge of the stone. Between two dates, the age is worked out from the depth.

14,000 to 12,000 years ago

The colours change

Each band is coloured by how heavy the oxygen in that piece of stone is. Between 14,000 and 12,000 years ago it gets heavier, one of the biggest shifts in the whole stone.

That is when the last ice age was giving way to the warm period we live in, which began about 11,700 years ago. The study’s summary says the oxygen varies with where the rain comes from and how much falls.

26,000 to 19,000 years ago

Ice at its biggest

When the ice sheets were at their largest, about 26,000 to 19,000 years ago, this stone in Brazil went on growing, about 5 to 6 millimetres every thousand years.

Zoomed out

A rhythm in the colours

Zoom out and the colours rise and fall in a slow rhythm. The pattern repeats about every 24,000 years. Chance alone would produce a repeat this clear about once in 70 times.

The study’s authors link these swings to summer sunlight, whose strength shifts as the direction of Earth’s axis slowly turns.

687 millimetres down

Where it began

The oldest date, 687 millimetres down, is 114,905 years, give or take 5,100. This is the bottom: everything above it, about 70 centimetres, arrived one drop at a time.

Averaged over its life, it grew about 6 millimetres in a thousand years.

Caves around the world

One of about 900 records

Scientists have gathered about 900 records like this one, from 365 caves, in one shared database. Each dot is a cave; Botuverá is the gold one.

Six caves

Six caves in Romania

Six of the caves are in Romania. How fast a stone grows depends on the cave, the rock and the water, so one stone says little about another.

One stalagmite from Cloșani Cave grew 46 centimetres in about 3,800 years, roughly 15 times faster than BT-2 grew over its last 2,300 years.

Pass it on

If you know someone who likes caves, deep time or very slow things, send them the page.

Sources and notes

What is measured and what is drawn. The depths, the ages, the dates with their margins and the colours are the stone’s own data (689 oxygen measurements; 20 uranium–thorium dates, plus the top, taken as still growing; every “give or take” is a 95% range). The outline, the width, the curved layers, the cave, the drops and the thin layers at the top are drawn. Colours between two measurements are blended, and the colour scale is stretched to the stone’s own spread (the 95th percentile of its distance from its average), so that its swings are easy to see. Ages are years before 1950, which at these scales is “years ago” to within a century. No one measured how often a drop falls in this cave, so the page gives no rate of dripping. The study’s title says 116,000 years; the stone was sampled slightly below its oldest date (687 millimetres, 114,905 ± 5,100 years), and the ages of those last centimetres are estimated from the dates above, so the page says 115,000. The database gives the first date as 2,245 years; the original study’s table gives about 2,350, and the page uses the database.

Your lifetime. The stone stopped growing when it was taken from the cave, so the sentence under your birth year says what a stone like this would have added at its recent rate, 8.3 millimetres per thousand years (between 7.9 and 8.8 if the dates are allowed their full 95% margin). Other stretches of this stone grew between 2.4 and 14 millimetres per thousand years.

The colours and the rhythm. Lighter or heavier oxygen is the quantity measured (δ18O). The study’s summary links it to the source and amount of rain at this site; other caves differ. The shift between 14,000 and 12,000 years ago is 2.2 parts per thousand, comparing 1,000-year means. The 24,000-year repeat is the strongest peak of the stone’s own series; random series with the same slow drift produce a peak that strong about once in 70 times (p = 0.014).

  1. Kaushal, N. et al. (2024). “SISALv3: a global speleothem stable isotope and trace element database.” Earth System Science Data 16, 1933–1963. Data: Oxford Research Archive, version 3, licence CC BY 4.0. Every depth, age, date, oxygen value and site on the page, and the counts of caves and stones.
  2. Cruz, F. W. et al. (2005). “Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil.” Nature 434, 63–66. The stalagmite BT-2 and its record. The study’s summary, as reproduced in NOAA’s data file, says the oxygen varies with the source and amount of rain, driven mainly by summer sunlight; 20 U/Th ages.
  3. Walker, M. et al. (2009). “Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records.” Journal of Quaternary Science 24, 3–17. The start of the warm period, about 11,700 years ago.
  4. Clark, P. U. et al. (2009). “The Last Glacial Maximum.” Science 325, 710–714. Ice sheets at their biggest, about 26,000 to 19,000 years ago.
  5. Credit card thickness 0.76 mm: ISO/IEC 7810, card format ID-1. Closani stalagmite C09-2: Warken, S. F. et al. (2018), “Reconstruction of late Holocene autumn/winter precipitation variability in SW Romania from a high-resolution speleothem trace element record.” Earth and Planetary Science Letters 499, 122–133 (the stone and its ages come from the database). Relief of the world map: NOAA, ETOPO 2022 Global Relief Model.