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Presentation given at the EGU conference in Vienna April 13-18 2008
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Presentation given at the GSA annual meeting in Houston TX October 5-9 2008
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Presentation about my PhD research, given at the bivalve workshop in Brussels in May 2009.
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Presentation about my PhD research, given at the Australian National University in May 2007.
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Presentation given at the GSA annual meeting in Houston TX October 5-9 2008
Gsa Houston 2008
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Presentation about my PhD research, given at the bivalve workshop in Brussels in May 2009.
Bivalve workshop May 2009
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Presentation about my PhD research, given at the Australian National University in May 2007.
Australia
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Global Climate Change- THE EFFECTS
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Field lab2
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Press release distribution service antarctica
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Seminar given at UC Santa Cruz in their Whole Earth seminar series.
UC Santa Cruz
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Emma Versteegh
Poster presented at JPL postdoc research day.
Previously unsuspected dietary habits of Rimicaris hybisae
Previously unsuspected dietary habits of Rimicaris hybisae
Emma Versteegh
Previously unsuspected dietary habits of hydrothermal vent fauna: the bacterivorous shrimp Rimicaris hybisae can be carnivorous
Poster EGU2014
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Emma Versteegh
Two hydrothermal vent fields have been described at the ultra-slow spreading ridge of the Mid-Cayman Rise (MRC), including the world’s deepest (Piccard ~4985m) and the nearby Von Damm vent field (~2300m). Both vent fields support a localized high-biomass. The food web has chemoautotrophic bacteria at the base and includes bacterivorous shrimp as well as carnivores: shrimp and anemones. The alvinocaridid shrimp Rimicaris hybisae is abundant at both vent fields and shows spatial variability in population structure. So far it has been considered bacterivorous. Large variations in tissue δ13C values remained largely unexplained, and it has been argued that δ13C values are not a good food web tracer in hydrothermal vent ecosystems. We observed that shrimp tended to be either in dense aggregations on active chimneys, or more sparsely distributed and peripheral in (near) ambient temperatures. With the hypotheses that varying δ13C values show real differences in food sources and that shrimp in different locales might have different diets, we collected shrimp from both environments at the Von Damm site during an Ocean Exploration Trust Expedition with E/V Nautilus (NA034, 08/2013) and examined their gut contents. Gut contents of all shrimp from dense aggregations consisted of white, amorphous material that resembled bacteria. Sparsely distributed shrimp (~1m from dense aggregations) had guts filled with fragments of crustacean exoskeleton, a mixture of bacteria-like material and crustacean exoskeleton, or bacteria-like material only. We analyzed stable isotope compositions of the shrimp and their gut contents. Shrimp δ13C, δ15N and δ34S values reflect those of their gut contents +1 trophic level. Sparse shrimp have dramatically lower δ13C and δ34S values, and slightly elevated δ15N values, in comparison to dense shrimp. Sparse and dense R. hybisae clearly have different diets. Ongoing work is determining what exactly is this crustacean food source, whether diet changes occur during life history, and if this is linked to the molting cycle.
Versteegh Goldschmidt 2014
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The world’s deepest hydrothermal vents: An analog for Europa?
The world’s deepest hydrothermal vents: An analog for Europa?
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Presentation given with Mark at the Oxfordshire Science Festival
Time travelling to climates of the past
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Presentation given at the Goldschmidt Conference in Florence
Goldschmidt 2013
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Seminar given for the department in Reading.
Seminar Silent Witnesses
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What are Marine Isotope Stages? How can MIS data be collected and what can we infer from them? Find out all about MIS in this presentation.
Marine isotope stages
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Climate change part 1
Climate change part 1
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Climate change part 1
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A Stable Isotopic Record for the Badlands National Park was obtained across the Eocene-Oligocene Transition (Greenhouse to Icehouse global climate change). The isotopic record indicates changes in temperature and aridity and allows for direct comparision of a local continental climate response to a global climate change event. Effect on regional biota are also described. This presentation was given at the GSA North-Central/South-Central Combined Meeting 2010.
Global Climate Change Effects on the Mid-Continent
Global Climate Change Effects on the Mid-Continent
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Climate change isotopes and ice house
Climate change isotopes and ice house
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Presented at the 2nd International Sclerochronology Conference, July 2010, Mainz Germanny.
ISC2010
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A stable isotopic record was obtained from paleosols in the Badlands National Park across the Chadronian-Orellan NALMA (Eocene-Oligocene). Results indicate a decoupling of the terrestrial and marine responses to global climate change. Tectonic forces and micro-climate regimes appear to have a strong influencing role in the mid-continent. This presentation represents the Defense for the degree of Master of Science in Geology, November 10, 2010.
Badlands National Park Isotopic Record of Climate Change Across the Eocene-Ol...
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Ostermann-Oceanus-2
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Microfossil importance in temparature 13
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Bibek Chatterjee
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climate change in the past: Palaeoclimate
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Annually Laminated Speleothems: Implications for Paleoclimate
Speleothems Ppt
Speleothems Ppt
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Basic principles of Paleoclimate and Paleoenvrironmental analysis.pptx
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Seminar given at UC Santa Cruz in their Whole Earth seminar series.
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Emma Versteegh
Poster presented at JPL postdoc research day.
Previously unsuspected dietary habits of Rimicaris hybisae
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Emma Versteegh
Previously unsuspected dietary habits of hydrothermal vent fauna: the bacterivorous shrimp Rimicaris hybisae can be carnivorous
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Emma Versteegh
Two hydrothermal vent fields have been described at the ultra-slow spreading ridge of the Mid-Cayman Rise (MRC), including the world’s deepest (Piccard ~4985m) and the nearby Von Damm vent field (~2300m). Both vent fields support a localized high-biomass. The food web has chemoautotrophic bacteria at the base and includes bacterivorous shrimp as well as carnivores: shrimp and anemones. The alvinocaridid shrimp Rimicaris hybisae is abundant at both vent fields and shows spatial variability in population structure. So far it has been considered bacterivorous. Large variations in tissue δ13C values remained largely unexplained, and it has been argued that δ13C values are not a good food web tracer in hydrothermal vent ecosystems. We observed that shrimp tended to be either in dense aggregations on active chimneys, or more sparsely distributed and peripheral in (near) ambient temperatures. With the hypotheses that varying δ13C values show real differences in food sources and that shrimp in different locales might have different diets, we collected shrimp from both environments at the Von Damm site during an Ocean Exploration Trust Expedition with E/V Nautilus (NA034, 08/2013) and examined their gut contents. Gut contents of all shrimp from dense aggregations consisted of white, amorphous material that resembled bacteria. Sparsely distributed shrimp (~1m from dense aggregations) had guts filled with fragments of crustacean exoskeleton, a mixture of bacteria-like material and crustacean exoskeleton, or bacteria-like material only. We analyzed stable isotope compositions of the shrimp and their gut contents. Shrimp δ13C, δ15N and δ34S values reflect those of their gut contents +1 trophic level. Sparse shrimp have dramatically lower δ13C and δ34S values, and slightly elevated δ15N values, in comparison to dense shrimp. Sparse and dense R. hybisae clearly have different diets. Ongoing work is determining what exactly is this crustacean food source, whether diet changes occur during life history, and if this is linked to the molting cycle.
Versteegh Goldschmidt 2014
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Emma Versteegh
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The world’s deepest hydrothermal vents: An analog for Europa?
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Previously unsuspected dietary habits of Rimicaris hybisae
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Poster EGU2014
Poster EGU2014
Versteegh Goldschmidt 2014
Versteegh Goldschmidt 2014
The world’s deepest hydrothermal vents: An analog for Europa?
The world’s deepest hydrothermal vents: An analog for Europa?
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What are Marine Isotope Stages? How can MIS data be collected and what can we infer from them? Find out all about MIS in this presentation.
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Climate change part 1
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A Stable Isotopic Record for the Badlands National Park was obtained across the Eocene-Oligocene Transition (Greenhouse to Icehouse global climate change). The isotopic record indicates changes in temperature and aridity and allows for direct comparision of a local continental climate response to a global climate change event. Effect on regional biota are also described. This presentation was given at the GSA North-Central/South-Central Combined Meeting 2010.
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A stable isotopic record was obtained from paleosols in the Badlands National Park across the Chadronian-Orellan NALMA (Eocene-Oligocene). Results indicate a decoupling of the terrestrial and marine responses to global climate change. Tectonic forces and micro-climate regimes appear to have a strong influencing role in the mid-continent. This presentation represents the Defense for the degree of Master of Science in Geology, November 10, 2010.
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Goldschmidt 2012 - Earth in Evolution, June 24-29, Montreal, Canada. Earthworm secreted calcium carbonate - a new palaeothermometer?
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Talk about life on Mars, given at the OK 2010 astronomical youth camp.
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Talk about the Pioneer effect. Given at the OK 2005 astronomical youth camp.
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Talk about Meteorite impacts and mass extinctions given at the Wika 2005 astronomy youth camp.
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Talk about the human eye. Given at the Roka 1999 astronomical youth camp in Romania.
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Egu2008
1.
Stable oxygen isotopes
in freshwater mussels (Unionidae) as a proxy for late Holocene floods and droughts of Rhine and Meuse Emma Versteegh Hubert Vonhof Simon Troelstra Dick Kroon
2.
3.
Stable oxygen isotopes
4.
Rivers Rhine and
Meuse
5.
δ 18 O
rivers Glacier melting High discharge Flood Dry summer
6.
7.
8.
9.
10.
11.
Late Holocene shells
12.
Palaeogeography
13.
Results Average
δ 18 O per shell
14.
Seasonal patterns Slowing
down of growth
15.
20 th
century shells
16.
17.
Measured δ
18 O vs. Predicted δ 18 O
18.
Measured δ
18 O vs. Predicted δ 18 O: 20 th century shells Juvenile stage
19.
Measured δ
18 O vs. Predicted δ 18 O: 20 th century shells Glacier melting Dry summer ???
20.
Measured δ
18 O vs. Predicted δ 18 O: monitoring
21.
Late Holocene shells
22.
23.