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136. Khozyem H, Adatte T, Keller G, Tantawy AA, Spangenberg JE (2014) The paleocene-eocene
GSSP at Dababiya, Egypt-Revisited. Episodes 37(2):78–86
137. Khozyem H, Adatte T, Spangenberg EJ, Tantawy A, Gerta Keller K (2013) Paleoenvironmental and climatic changes during the Paleocene-Eocene thermal maximum (PETM) at the
Wadi Nukhul Section, Sinai, Egypt. J Geol Soc Lond 170:341–352
138. Khozyem H, Adatte T, Spangenberg JE, Keller G, Tantawy AA, Ulianov A (2015) New
geochemical constraints on the Paleocene-Eocene thermal maximum: Dababiya GSSP, Egypt.
Palaeogeogr Palaeoclimatol Palaeoecol 429:117–135
139. Castree N (2015) The Anthropocene: a primer for geographers. Geography 100 part 2: 66
140. Edwards LE (2015) What is the Anthropocene? Eos 96. https://doi.org/10.1029/
2015eo040297
141. Waters CN, Zalasiewicz J, Summerhayes C, Fairchild IJ, Rose NL, Loader NJ, Shotyk W,
Cearreta A, Head MJ, James PM, Syvitski, Williams M, Wagreich M, Barnosky AD, Zhisheng
A, Leinfelder R, Jeandel C, Gałuszka A, Ivar do Sul JA, Gradstein F, Steffen W, McNeill JR,
Wing S, Poirier C, Edgeworth M (2017) Global boundary stratotype section and point (GSSP)
for the Anthropocene Series: where and how to look for potential candidates. https://doi.org/
10.1016/j.earscirev.2017.12.016
142. Waters CN et al (2016) The Anthropocene is functionally and stratigraphically distinct from
the Holocene. Science 351(6269). https://doi.org/10.1126/science.aad2622
143. Mason B (2003) Man has been changing climate for 8,000 years. Nature. https://doi.org/10.
1038/news031208-7
144. Ruddiman WF (2003) The anthropogenic greenhouse era began thousands of years ago. Clim
Change 61(3):261–293. https://doi.org/10.1023/b:clim.0000004577.17928.fa
145. ESRL Web Tea (2015) ESRL global monitoring division–global greenhouse gas reference
network. noaa.gov
146. NASA (2016) Global climate change—vital signs of the planet—facts—Carbon Dioxide
147. Lewis SL, Maslin MA (2015) Defining the Anthropocene (PDF). Nature 519(7542):171–180.
https://doi.org/10.1038/nature14258
148. Keller G, Mateo P, Punekar J, Khozyem H, Gertsch B, Spangenberg JE, Font E, Bitchong
A, Adatte T (2018) Environmental changes across the Cretaceous-Paleogene mass extinction
and paleocene-eocene thermal maximum: implications for the anthropocene. Gondwana Res
56:69–89. https://doi.org/10.1016/j.gr.2017.12.002
H. Khozyem
131. Dupuis C, Aubry M-P, Steurbaut E, Berggren WA, Ouda K, Magioncalda R, Cramer BS, Kent
DV, Speijer RP, Heilmann-Clausen C (2003) The Dababiya Quarry section: lithostratigraphy,
clay mineralogy, geochemistry and paleontology. In: Ouda K, Aubry M-P (eds) The upper
Paleocene–Lower Eocene of the Upper Nile Valley: Part 1. Stratigraphy: micropaleontology,
vol 49, pp 41–59
132. Jaramillo CA, Ochoa D, Contreras L, Pagani M, Carvajal-Ortiz H et al (2010) Effects of
rapid global warming at the Paleocene-Eocene boundary on neotropical vegetation. Science
330:957–961
133. Aziz HA, Hilgen FJ, Luijk GM, Sluijs A, Kraus MJ (2008) Astronomical climate control
on paleosol stacking patterns in the upper Paleocene-lower Eocene Willwood Formation,
Bighorn Basin, Wyoming. Geology 36:531–534
134. Röhl U, Westerhold T, Bralower TJ, Zachos JC (2007) On the duration of the PaleoceneEocene thermal maximum (PETM). Geochem Geophys Geosyst 8, Q12002 pp
135. Murphy BH, Farley KA, Zachos JC (2010) An extraterrestrial 3He-based timescale for the
Paleocene-Eocene thermal maximum (PETM) from Walvis Ridge, IODP Site 1266. Geochim
Cosmochim Acta 74:5098–5108
136. Khozyem H, Adatte T, Keller G, Tantawy AA, Spangenberg JE (2014) The paleocene-eocene
GSSP at Dababiya, Egypt-Revisited. Episodes 37(2):78–86
137. Khozyem H, Adatte T, Spangenberg EJ, Tantawy A, Gerta Keller K (2013) Paleoenvironmental and climatic changes during the Paleocene-Eocene thermal maximum (PETM) at the
Wadi Nukhul Section, Sinai, Egypt. J Geol Soc Lond 170:341–352
138. Khozyem H, Adatte T, Spangenberg JE, Keller G, Tantawy AA, Ulianov A (2015) New
geochemical constraints on the Paleocene-Eocene thermal maximum: Dababiya GSSP, Egypt.
Palaeogeogr Palaeoclimatol Palaeoecol 429:117–135
139. Castree N (2015) The Anthropocene: a primer for geographers. Geography 100 part 2: 66
140. Edwards LE (2015) What is the Anthropocene? Eos 96. https://doi.org/10.1029/
2015eo040297
141. Waters CN, Zalasiewicz J, Summerhayes C, Fairchild IJ, Rose NL, Loader NJ, Shotyk W,
Cearreta A, Head MJ, James PM, Syvitski, Williams M, Wagreich M, Barnosky AD, Zhisheng
A, Leinfelder R, Jeandel C, Gałuszka A, Ivar do Sul JA, Gradstein F, Steffen W, McNeill JR,
Wing S, Poirier C, Edgeworth M (2017) Global boundary stratotype section and point (GSSP)
for the Anthropocene Series: where and how to look for potential candidates. https://doi.org/
10.1016/j.earscirev.2017.12.016
142. Waters CN et al (2016) The Anthropocene is functionally and stratigraphically distinct from
the Holocene. Science 351(6269). https://doi.org/10.1126/science.aad2622
143. Mason B (2003) Man has been changing climate for 8,000 years. Nature. https://doi.org/10.
1038/news031208-7
144. Ruddiman WF (2003) The anthropogenic greenhouse era began thousands of years ago. Clim
Change 61(3):261–293. https://doi.org/10.1023/b:clim.0000004577.17928.fa
145. ESRL Web Tea (2015) ESRL global monitoring division–global greenhouse gas reference
network. noaa.gov
146. NASA (2016) Global climate change—vital signs of the planet—facts—Carbon Dioxide
147. Lewis SL, Maslin MA (2015) Defining the Anthropocene (PDF). Nature 519(7542):171–180.
https://doi.org/10.1038/nature14258
148. Keller G, Mateo P, Punekar J, Khozyem H, Gertsch B, Spangenberg JE, Font E, Bitchong
A, Adatte T (2018) Environmental changes across the Cretaceous-Paleogene mass extinction
and paleocene-eocene thermal maximum: implications for the anthropocene. Gondwana Res
56:69–89. https://doi.org/10.1016/j.gr.2017.12.002