Global warming and the Late Permian mass extinction event
Lead Research Organisation:
Plymouth University
Department Name: Sch of Earth Ocean and Environment
Abstract
Life on Earth has been affected by a number of mass extinction events, where a significant proportion of the animals and plants, on land and in the sea, disappeared forever. One well-known example is the extinction event that wiped out the dinosaurs at the end of the Cretaceous Period, 65 million years ago. The end-Cretaceous event is dwarfed, however, by the most severe mass extinction event recorded in the fossil record: the Late Permian event. The Late Permian event happened just over 250 million years ago, during which time at least 80% and perhaps more than 90% of species in the oceans and on land became extinct. In recent years an increasing number of scientists have started to investigate this important event in earth history. There is still much that we do not know, especially regarding the cause(s) of the catastrophe. There is no good evidence of a meteorite impact at that time, but the event does seem to coincide with the largest outpourings of volcanic lava on land which occurred in present-day Siberia. Most scientists now think that the volcanic eruptions in Siberia released carbon dioxide that slowly built up in the atmosphere. Carbon dioxide is a well-known greenhouse gas. As temperatures began to rise, scientists think that the Earth suffered a 'runaway greenhouse' and global warming spiralled out of control. Scientists estimate that the huge loss of life occurred during a time when global temperatures rose by 5-6 degress C, which is in the upper range of predictions made for temperature increase in the next century. There are, however, potential problems with this 5-6 degree temperature estimate. The numbers derive from geochemical studies of limestone rocks from southern Austria made in the late 1980s. Unfortunately, these rocks are not very well preserved, and with our modern understanding of geochemistry we now think that these estimates are wrong. We need to find an alternative way of estimating temperature change in the past. One way is to analyse the shells from fossil marine animals called brachiopods. The geochemical signature of the seawater in which these animals lived is preserved within their shells, and from analysis of well-preserved shells we can reconstruct the temperature of the ancient seawater. There are two types of brachiopod: inarticulate and articulate. The articulate brachiopods were very common in the Permian, but much rarer today, and their calcite shells are often used to reconstruct past climate. The inarticulates include the brachiopod Lingula, which is a 'living fossil', having survived the major extinction events of the past. Lingula is very common before and especially just after the Late Permian extinction event. Recent work has shown for the first time that parts of the Lingula shell (the portion made of calcite) also preserve the geochemical signature of the seawater in which the animal lived. Until now, nobody has used Lingula to reconstruct past climate. We will collect brachiopods from just before and just after the extinction event from northern Italy. We already know, from preliminary work, that the rocks are well exposed there, contain abundant fossil brachiopods, and that the brachiopods are well-preserved. Using geochemical techniques we will examine the preservation of each fossil shell we collect, and will use the best preserved ones to produce estimates of the water temperatures in which the animals actually lived. We expect to see a change through the extinction event, but will it be a rise of 5-6 degrees? Perhaps the temperature change was more, or less, severe than scientists presently think. This important information will help improve our understanding of the greatest mass extinction event in our planet's history and will help improve our understanding of past climate change.
Organisations
Publications
Kearsey T
(2009)
Isotope excursions and palaeotemperature estimates from the Permian/Triassic boundary in the Southern Alps (Italy)
in Palaeogeography, Palaeoclimatology, Palaeoecology
Metcalfe B
(2011)
Changes in size and growth rate of 'Lilliput' animals in the earliest Triassic
in Palaeogeography, Palaeoclimatology, Palaeoecology
Price GD
(2013)
Isotopic evidence for long term warmth in the Mesozoic.
in Scientific reports
Price GD
(2010)
Evaluating CO2 as a primary driver of Paleozoic-Mesozoic climate change
in Geological Society of America Abstracts with Programs
Description | RT: Marie Curie Intra-European Fellowship grant EMBiCC |
Amount | € 172,434 (EUR) |
Funding ID | 237449 |
Organisation | Marie Sklodowska-Curie Actions |
Sector | Charity/Non Profit |
Country | Global |
Start | 05/2009 |
End | 04/2011 |
Description | Manchester GA talk |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | No |
Geographic Reach | Local |
Primary Audience | Public/other audiences |
Results and Impact | Invited lecture to discuss past global warming and extinctions |
Year(s) Of Engagement Activity | 2016 |
Description | Twitchett RJ: 25th Anniversary Talk of the Cambridgeshire Geology Club |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | No |
Geographic Reach | Local |
Primary Audience | Public/other audiences |
Results and Impact | Talk title: Turning up the heat on the Late Permian extinction event. Talk sparked questions and discussion After my talk audience members reported that they enjoyed hearing about the latest developments in the science that previously they were unaware of. |
Year(s) Of Engagement Activity | 2007,2011 |
Description | Twitchett RJ: Christmas Science Lecture, St Boniface's College, Plymouth, UK |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | No |
Geographic Reach | Local |
Primary Audience | Schools |
Results and Impact | Talk sparked questions and discussion, and interest in show-and-tell specimens After my talk teachers and pupils expressed enjoyment at learning something new about the past and implications for the future of the world's oceans |
Year(s) Of Engagement Activity | 2010 |
Description | Twitchett RJ: SW Regional Group talk (Torbay school) |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | No |
Geographic Reach | Regional |
Primary Audience | Public/other audiences |
Results and Impact | Talk title: mass extinction. Talk sparked questions and discussion After the activity audience members expressed enjoyment at learning about something new |
Year(s) Of Engagement Activity | 2011 |
Description | Twitchett: Dorset County Museum talk |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | No |
Geographic Reach | Local |
Primary Audience | Public/other audiences |
Results and Impact | Talk sparked questions and discussion afterwards After the talk on global warming and mass extinction events, the audience expressed enjoyment at learning more about the past and its implications for the future |
Year(s) Of Engagement Activity | 2013 |
Description | Twitchett: MBA seminar |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | No |
Geographic Reach | Local |
Primary Audience | Other academic audiences (collaborators, peers etc.) |
Results and Impact | talk sparked questiosn and discussion afterwards potential future collaborations explored |
Year(s) Of Engagement Activity | 2009 |
Description | Yorks Fossil Festival 2016 |
Form Of Engagement Activity | Participation in an activity, workshop or similar |
Part Of Official Scheme? | No |
Geographic Reach | Regional |
Primary Audience | Public/other audiences |
Results and Impact | During the Fossil Festival weekend, ca. 220 children and their parents engaged with my novel game that involved learning about the effects of climate change on marine animals ('Extinction Kerplunk') |
Year(s) Of Engagement Activity | 2016 |