Dropstone

Examples of dropstones from the Eocene, when it has been suggested that there were no ice sheets.^[1]

Dropstones are isolated fragments of rock found within finer-grained water-deposited sedimentary rocks. They range in size from small pebbles to boulders. The critical distinguishing feature is that there is evidence that they were not transported by normal water currents, but rather dropped in vertically through the water column.

Background

When deposited into fine layered mud, such evidence includes an impact depression beneath the dropstone, and indication that the mud has been squeezed up around the edges of the falling rock. Subsequent deposits of mud drape over the dropstone and its crater. Glacial dropstones, involving rocks falling out of icebergs, are one of the most common types of dropstone preserved in the geological record, particularly when deposited in low-energy deep sea or lake environments. Dropstones differ from erratics found in glacial till in that they are deposited in a lake or marine environments. Dropstones may also be deposited by a variety of non-glacial means.

Origin of dropstones

There are four natural mechanisms that produce dropstones:

Glacial dropstone from Permian rocks in eastern Australia

Glaciers

As glaciers move across a surface, they pluck rocks from it, and incorporate them into their mass. At the coast, fragments of glacier detach and float away as icebergs, which are often transported (ice rafted) many miles into the ocean, where they melt and deposit their load. When entrained rocks sink to the ocean floor, they can be incorporated into the oceanic sediments, which are typically fine grained.

Volcanoes

Whilst dropstones were once thought to be diagnostic of glaciers, it has since been realised that they can also be formed via volcanic eruptions. Volcanic 'bombs' are large fragments of rock, projected many miles by the force of an eruption. If these land in fine sediments, they can form dropstones.^[2] Dropstones originating in this fashion are relatively rare in the geological record as most will invariably land on high ground, which has a poor preservation potential as it is in an erosive environment. However, a large blast may spread bombs far enough for them to end up in a marine setting of fine enough sediment for them to be recognised.

Turbidity currents

Dropstones can also be deposited through the action of strong ocean-floor turbidity currents.^[3] Boulders the size of a man have been found in relatively recent finely laminated sediments near Jamaica,^[4] which has been a warm tropical island entirely devoid of glaciers since it came into existence.^[5] Whilst turbidity currents are cited as the origin of the boulders, they are not found in association with deposits formed by them.

Biological rafts

Examples of gastrolith dropstones from the Tropic Shale (Cretaceous) of Utah.

Stones can also be transported large distances by becoming bound in a raft of floating plant material or in the roots of floating trees.^[6] When such a raft disintegrates due to waterlogging and sinking of its constituents, the transported rocks would also sink. Dropstones formed in this manner are typically associated with organic matter, especially logs - the fossilised remains of the raft that caused its transport.

Vertebrates may also act as "rafts" by ingesting gastroliths and depositing them in standing bodies of water by regurgitation or when the organism dies^[6].

See also

• Ice rafting
• Glacial erratic

References

1. ^ Image reproduced under license from Eldrett, J.S.; Harding, I.C., Wilson, P.A., Butler, E., Roberts, A.P. (2007). "Continental ice in Greenland during the Eocene and Oligocene" (^{[dead link]} – ^{Scholar search}). Nature 446 (7132): 176. doi:10.1038/nature05591. PMID 17287724. http://www.nature.com/nature/journal/vaop/ncurrent/full/nature05591.html. Retrieved 2007-04-29. 
2. ^ Bennett, MR; Doyle, P., Mather, AE, Woodfin, JL (1994). "Testing the climatic significance of dropstones: an example from southeast Spain". Geological Magazine 131 (06): 845–848. doi:10.1017/S0016756800012917. 
3. ^ Bennett, MR; Doyle, P. (1996). "Global cooling inferred from dropstones in the Cretaceous: fact or wishful thinking?". Terra Nova 8 (2): 182–185. doi:10.1111/j.1365-3121.1996.tb00742.x. 
4. ^ Donovan, SK; Pickerill, RK (1997). "Dropstones: their origin and significance: a comment". Palaeogeography, Palaeoclimatology, Palaeoecology 131 (1): 175–178. doi:10.1016/S0031-0182(96)00150-2. http://www.sciencedirect.com/science?_ob=MImg&_imagekey=B6V6R-3SWK00R-9-1&_cdi=5821&_user=1495569&_orig=browse&_coverDate=06%2F30%2F1997&_sk=998689998&view=c&wchp=dGLbVzb-zSkzk&md5=57f0e6785dd8c41347bff2790a645880&ie=/sdarticle.pdf. Retrieved 2007-04-27. 
5. ^ Pindell, J. (1994). "Evolution of the Gulf of Mexico and the Caribbean". In Pindell, J., Donovan, S.K., Jackson, T.A.. Caribbean geology, an introduction. University of the West Indies Publishers Association/University of the West Indies Press, Kingston, Jamaica. 
6. ^ ^{a b} Bennett, MR; Doyle, P., Mather, AE (1996). "Dropstones: their origin and significance". Palaeogeography, Palaeoclimatology, Palaeoecology 121 (3): 331–339. doi:10.1016/0031-0182(95)00071-2. http://www.ingentaconnect.com/content/els/00310182/1996/00000121/00000003/art00071. Retrieved 2007-04-27. 

External links

Media related to Dropstones at Wikimedia Commons