Summary
Planktic microfossils arguably provide the most complete (stratigraphic and taxonomic) record of biodiversity of any group of organisms. The phytoplankton record is of particular significance as it most likely tracks global changes in the climate-ocean system and, in turn, influenced biodiversity and productivity of higher trophic levels of the biosphere. Coccolithophores and associated calcareous nannoplankton first appear in the fossil record in Upper Triassic sediments (~225 Ma) and, despite significant extinctions at the Triassic/Jurassic boundary, the Mesozoic diversity record is one of relatively uniform increase punctuated by short periods of turnover and decline. Rates of speciation that are significantly above background were restricted to the Late Triassic, Early Jurassic and Tithonian-Berriasian intervals. Enhanced rates of extinction occurred at the Triassic/Jurassic, Jurassic/Cretaceous and Cretaceous/Tertiary boundaries.
There is no clear correlation between coccolithophore diversity and Mesozoic climate, as it is currently understood, but the dominant trajectory of diversity increase suggests long-term stability and widespread oligotrophy in photic zone environments. The Neocomian and Campanian-Early Maastrichtian intervals of diversity increase are clearly associated with increased numbers of endemic taxa at both low and high latitudes. These intervals have been interpreted as periods of cooling or cooler climates, and greater differentiation of the photic zone environment may have led to the biogeographic partitioning. Notably, none of the mid-Cretaceous Oceanic Anoxic Events are associated with above-background evolutionary rates or significant taxonomic loss or innovation.
Cenozoic nannoplankton diversity patterns are markedly more variable than those of the Mesozoic, and rates of speciation, extinction and turnover are consistently higher. There is also good correlation between diversity and climate trends, with higher diversities associated with warm climates. This is best illustrated by the Paleogene record, where the Cenozoic diversity maximum, at the Paleo cene/Eocene boundary, coincided with climates of extreme warmth, and significant diversity decline tracked climate cooling through the Late Eocene and into the Oligocene. This relationship between climate and coccolithophore diversity is contrary to that observed in the Mesozoic, and suggests different controls on evolution during the two eras. The Cretaceous record suggests that cooling within a greenhouse-mode climate system may have stimulated diversification at all viable latitudes via biogeographic partitioning. In contrast, the Cenozoic data indicates that cooling tended to drive diversity decrease. This may be explained by the greater magnitude and longevity of Cenozoic cooling, in an icehouse-mode climate system, which prevented coccolithophore diversification at higher latitudes where, instead, diatoms became established as the dominant group of phytoplankton.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Aubry M-P (1984) Handbook of Cenozoic calcareous nannoplankton, Book 1: Ortholithae (Discoasters). Micropaleontology Press, American Museum of Natural History, New York
Aubry M-P (1988) Handbook of Cenozoic calcareous nannoplankton, Book 2: Ortholithae (Holococcoliths, Ceratoliths and others). Micropaleontology Press, American Museum of Natural History, New York
Aubry M-P (1989) Handbook of Cenozoic calcareous nannoplankton, Book 3: Ortholithae (Pentaliths, and others), Heliolithae (Fasciculiths, Sphenoliths and others). Micropaleontology Press, American Museum of Natural History, New York
Aubry M-P (1990) Handbook of Cenozoic calcareous nannoplankton, Book 4: Heliolithae (Helicoliths, Cribriliths, Lopadoliths and others). Micropaleontology Press, American Museum of Natural History, New York
Aubry M-P (1992) Late Paleogene calcareous nannoplankton evolution: a tale of climatic deterioration. In: Prothero DR, Berggren WA (eds) Eocene-Oligocene Climatic and Biotic Evolution, Princeton University Press, pp 272–309
Aubry M-P (1998) Early Paleogene calcareous nannoplankton evolution: a tale of climatic amelioration. In: Aubry M-P, Lucas SG, Berggren AW (eds) Late Paleocene-Early Eocene Climatic and Biotic Events in the Marine and Terrestrial Records. Columbia University Press, pp 158–203
Aubry M-P (1999) Handbook of Cenozoic calcareous nannoplankton, Book 4: Heliolithae (Zygoliths and Rhabdoliths). Micropaleontology Press, American Museum of Natural History, New York
Baumgartner PO (1987) Age and genesis of Tethyan Jurassic radiolarites. Eclogae Geol Helv 80: 831–879
Berggren WA, Kent DV, Swisher III CC, Aubry M-P (1995). A revised Cenozoic chronology and chronostratigraphy. In: Berggren WA, Kent DV, Hardenbol J (eds) Geochronology, Time-Scales, and Global Stratigraphie Correlation: Framework for an Historical Geology. SEPM Spec. Publ. 54: 129–212
Boersma A, Premoli Silva I (1991) Distribution of Paleogene planktonic foraminifera -analogies with the Recent? Palaeogeogr Palaeocl 83: 29–48
Bown PR (1987) Taxonomy, biostratigraphy, and evolution of late Triassic-early Jurassic calcareous nannofossils. Spec Pap Palaeontol 38: 1–118
Bown PR (1993) New holococcoliths from the Toarcian-Aalenian (Jurassic) of northern Germany. Senckenbergiana Lethaea 73: 407–419
Bown PR (1998a) Calcareous nannofossil biostratigraphy. Kluwer Academic Publishers, pp 1–315
Bown PR (1998b) Triassic. In: Bown PR (ed) Calcareous nannofossil biostratigraphy, Kluwer Academic Publishers, pp 29–33
Bown PR, Young JR (1997) Mesozoic calcareous nannoplankton classification. J Nannoplankton Res 19:21–36
Bown PR, Burnett JA, Gallagher LT (1991) Critical events in the evolutionary history of calcareous nannoplankton. Historical Biology 5: 279–290
Bown PR, Burnett JA, Gallagher LT (1992) Calcareous nannoplankton evolution. Memorie di Scienze Geologiche XLIII: 1–17
Bralower TJ, Arthur MA, Leckie RM, Sliter WV, Allard DJ, Schlanger SO (1994) Timing and paleoceanography of oceanic dysoxia/anoxia in the Late Barremian to Early Ap-tian (Early Cretaceous). Palaios 9: 335–369
Burnett JA (1998) Upper Cretaceous. In: Bown PR (ed) Calcareous nannofossil biostratigraphy. Kluwer Academic Publishers, pp 132–199
Burnett JA, Young JR, Bown PR (2000) Calcareous nannoplankton and global climate change. In: Culver S J, Rawson PF (eds) Biotic Response to Global Change: The last 145 million years. Cambridge University Press, pp 35–50
Chapman MR, Chepstow-Lusty AJ (1997) Late Pliocene climatic change and the global extinction of the discoasters: an independent assessment using oxygen isotope records. Palaeogeogr Palaeocl 134: 109–125
Chepstow-Lusty AJ, Shackleton NJ, Backman J (1992) Upper Pliocene Discoaster abundance variations from the Atlantic, Pacific and Indian Oceans: the significance of productivity pressure at low latitudes. Memorie di Scienze Geologiche XLIV: 357–373
Cros L, Kleijne A, Zeltner A, Billard C, Young JR (2000) New examples of holococcolith-heterococcolith combination coccospheres and their implications for coccolithophorid biology. Mar Micropaleontol 39: 1–34
Danelian T, Johnson KG (2001) Patterns of biotic change in Middle Jurassic to Early Cretaceous Tethyan radiolaria. Mar Micropaleontol 43: 239–260
Erba E (1994) Nannofossils and superplumes: The early Aptian “nannoconid crisis”. Paleoceanography 9: 483–501
Frakes LA (1999) Estimating the global thermal state from Cretaceous sea surface and continental temperature data. In: Barrera E, Johnson CC (eds) Evolution of the Cretaceous Ocean-Climate System. Geol Soc Am Spec Pap 332: 49–57
Frakes LA, Francis JE, Syktus JI (1992) Climate Modes of the Phanerozoic. Cambridge University Press, pp 1–274
Gale AS (2000) The Cretaceous World. In: Culver SJ, Rawson PF (eds) Biotic Response to Global Change: The last 145 million years. Cambridge University Press, pp 4–19
Gale AS, Smith AB, Monks NEA, Young JA, Howard A, Wray DS, Huggett JM (2000) Marine biodiversity through the Late Cenomanian-Early Turonian: palaeoceanographic controls and sequence stratigraphic biases. J Geol Soc London 157: 745–757
Gallois RW (1976) Coccolith blooms in the Kimmeridge Clay and the origin of North Sea Oil. Nature 259: 473–475
Gallois RW, Medd AW (1979) Coccolith-rich marker bands in the English Kimmeridge Clay. Geol Mag 116: 247–334
Gartner S (1996) Calcareous nannofossils at the Cretaceous-Tertiary boundary. In: MacLeod N, Keller G (eds) Cretaceous-Tertiary mass extinctions: biotic and environmental changes. W.W. Norton & Company, pp 27–47
Gould SJ, Gilinsky NL, German R (1987) Asymmetry of lineages and the direction of evolutionary time. Science 236: 1437–1441
Gradstein FM, Agterberg FP, Ogg JG, Hardenbol J, Van Veen P, Thierry J, Huang Z (1995) A Triassic, Jurassic and Cretaceous time-scale. In: Berggren WA, Kent DV, Hardenbol J(eds.), Geochronology, Time-Scales, and Global Stratigraphie Correlation: Framework for an Historical Geology. SEPM Spec Publ 54: 95–126
Hallam A, Wignall PB (1997) Mass extinctions and their aftermath. Oxford University Press, pp 320
Hailock P (1987) Fluctuations in the trophic resource continuum: A factor in global diversity cycles? Paleoceanography 2: 457–471
Hallock P, Premoli Silva I, Boersma A (1991) Similarities between planktonic and larger foraminiferal evolutionary trends through Paleogene paleoceanographic changes. Palaeogeogr Palaeocl 83: 49–64
Haq BU, Hardenbol J, Vail PR (1987) Chronology of Fluctuating Sea Levels Since the Triassic. Science 235: 1156–1167
Hesselbo SP, Robinson SA, Surlyk F, Piasecki S (2002) Terrestrial and marine extinction at the Triassic-Jurassic boundary synchronized with major carbon-cycle perturbation: a link to initiation of massive volcanism? Geology 30: 251–254
Huber BT (1998) Tropical paradise at the Cretaceous poles? Science 282: 2199–2200
Huber BT, Watkins DK (1992) Biogeography of Campanian-Maastrichtian calcareous plankton in the region of the Southern Ocean: paleogeographic and paleoclimatic implications. The Antarctic Paleoenvironment: a perspective on global change. Antarctic Research Series 56: 31–60
Janofske D (1992) Calcareous nannofossils of the Alpine Upper Triassic. In: Hamrsmîd B, Young JR (eds) Nannoplankton Research, Vol. 1, Knihovnicka ZPZ, 14a, 1: 87–109
Jenkyns HC, Gale AS, Corfield RM (1994) Carbon- and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic significance. Geol Mag 131: 1–34
Knoll A (1989) Evolution and extinction in the marine realm: some constraints imposed by phytoplankton. Phil Trans R Soc London B 325: 279–290
Leckie MR, Bralower TJ, Cashman R (2002) Oceanic anoxic events and plankton evolution: biotic response to tectonic forcing during the mid-Cretaceous. Paleoceanography, 17:1041
Lees JA (2002) Calcareous nannofossil biogeography illustrates palaeoclimate change in the late Cretaceous Indian Ocean. Cretaceous Res 23: 537–633
Lipps JH (1970) Plankton evolution. Evolution 24: 1–22
MacLeod N, Rawson PF, Forey PL, Banner FT, Boudagher-Fadel MK, Bown PR, Burnett JA, Chambers P, Culver S, Evans SE, Jeffery C, Kaminski MA, Lord AR, Milmer AC, Milner AR, Morris N, Owen E, Rosen BR, Smith AB, Taylor PD, Urquhart E, Young JR (1997) The Cretaceous-Tertiary biotic transition. J Geol Soc London 154: 265–292
McIntyre A, Bé AWH (1967) Modern Coccolithophoridae of the Atlantic Ocean. I. Placoliths and cyrtoliths. Deep-Sea Res 14: 561–597
Medlin LK, Kooistra WHCF, Potter D, Saunders JB, Andersen RA (1997) Phylogenetic relationships of the “golden algae” (haptophytes, heterokont chromophytes) and their plastids. Plant Syst Evol Supplementum 11: 187–219
Miller A (2000) Conversations about Phanerozoic global diversity. Paleobiology 26 (4) supplement, Deep Time: Paleobiology’s Perspective, pp 53–73
Okada H, Honjo S (1973) The distribution of oceanic coccolithophorids in the Pacific. Deep-Sea Res 20: 355–374
Olsen PE, Kent DV, Sues H-D, Koeberl C, Huber H, Montanari A, Rainforth EC, Fowell SJ, Szajna MJ, Hartline BW (2002) Ascent of dinosaurs linked to an iridium anomaly at the Triassic-Jurassic boundary. Science 296: 130–133
Perch-Nielsen K (1985a) Mesozoic calcareous nannofossils. In: Bolli HM, Saunders JB, Perch-Nielsen K (eds) Plankton Stratigraphy. Cambridge University Press, pp 329–426
Perch-Nielsen K (1985b) Cenozoic calcareous nannofossils. In: Bolli HM, Saunders JB, Perch-Nielsen K (eds) Plankton Stratigraphy. Cambridge University Press, pp 427–554
Perch-Nielsen K (1986) Geologic events and the distribution of calcareous nannofossils -some speculations. Bull Cent Rech Elf Aquitaine 10: 421–432
Pospichal JJ (1994) Calcareous nannofossils at the K-T boundary, El Kef: No evidence for stepwise, gradual, or sequential extinctions. Geology 22: 99–102
Pospichal JJ (1996) Calcareous nannoplankton mass extinction at the Cretaceous/Tertiary boundary: an update. In: Ryder G, Fastovsky D, Gartner S (eds) The Cretaceous-Tertiary event and other catastrophes in Earth history. Geol Soc Am Spec Paper 307: 335–360
Pospichal JJ, Wise SW Jr. (1990) Paleocene to Middle Eocene calcareous nannofossils of ODP Sites 689 and 690, Maud Rise, Weddell Sea. Proc Ocean Drill Prog Sci Results 113:613–638
Romein AJT (1979) Lineages in early Paleogene calcareous nannoplankton. Utrecht Micropaleontological Bulletins 22: 1–230
Roth PH (1986) Mesozoic palaeoceanography of the North Atlantic and Tethys Oceans. In: Summerhayes CP, Shackleton NJ (eds) North Atlantic Palaeoceanography. Geol Soc Spec Pub 21: 299–320
Roth PH (1987) Mesozoic calcareous nannofossil evolution: relation to paleoceanographic events. Paleoceanography 6: 601–611
Roth PH (1989) Ocean circulation and calcareous nannoplankton evolution during the Jurassic and Cretaceous. Palaeogeogr Palaeocl 74: 111–126
Savin SM, Abel L, Barrera E, Hodell D, Keller G, Kennett JP, Killingley J, Murphy M, Vincent E (1985) The evolution of Miocene surface and near-surface marine temperatures: oxygen isotopic evidence. In: Kennett JP (ed) The Miocene Ocean: paleoceanography and biogeography. Geol Soc Am Mem 163: 49–82
Sepkowski Jr. JJ (1978) A kinetic model of Phanerozoic taxonomic diversity. I. Analysis of marine orders. Paleobiology 4: 223–251
Sheridan RE, Gradstein FM et al. (1983) Init. Repts. DSDP, 76. Washington (US Govt. Printing Office)
Siesser WG (1998) Calcareous nannofossil genus Scyphosphaera: structure, taxonomy, biostratigraphy, and phylogeny. Micropaleontology 44: 351–384
Smith A (1994) Systematics and the fossil record. Blackwell, 223pp
Spencer-Cervato C (1999) The Cenozoic Deep Sea Microfossil Record: Explorations of the DSDP/ODP Sample Set Using the Neptune Database. Palaeontologica Electronica, 2: art. 4
Sprengel C, Young JR (2000) First direct documentation of associations of Ceratolithus cristatus ceratoliths, hoop-coccoliths and Neosphaera coccolithomorpha planoliths. Mar Micropaleontol 3: 39–41
Stover LE, Brinkhuis H, Damassa SP, de Verteuil L, Helby RJ, Monteil E, Partridge AD, Powell AJ, Riding JB, Smelror M, Williams GL (1996) Mesozoic-Tertiary dinoflag-ellates, acritarchs and prasinophytes. In: Jansonius J, McGregor DC (eds) Palynology: principles and applications, vol 2. American Association of Stratigraphic Palynologists Foundation, pp 641–750
Tappan H, Loeblich Jr. AR (1973) Evolution of the Oceanic Plankton. Earth-Sci Rev 9: 207–240
Tappan H, Loeblich Jr. AR (1988) Foraminiferal evolution, diversification and extinction. J Paleontol 62: 695–741
Thierstein HR (1981) Late Cretaceous calcareous nannoplankton and the change at the Cretaceous-Tertiary boundary. In: Douglas RG, Warme J, Winterer EL (eds) The Deep Sea Drilling Project: a decade of progress. SEPM, Spec Pub 32: 355–394
Vermeij GJ (1995) Economics, volcanoes, and Phanerozoic revolutions. Paleobiology 21: 125–252
Watkins D, Wise S, Pospichal J, Crux J (1996) Upper Cretaceous calcareous nannofossil biostratigraphy and paleoceanography of the Southern Ocean. In: Moguilevsky A, Whatley R (eds) Microfossils and oceanic environments. University of Wales, Aber-ystwyth-Press,pp 355–381
Wei W, Kennett JP (1986) Taxonomic evolution of Neogene planktonic foraminifera and paleoceanographic relations. Paleoceanography 1: 67–84
Wignall PB (2001) Large igneous provinces and mass extinctions. Earth-Sci Rev 53: 1–33
Winter A, Jordan RW, Roth P (1994) Biogeography of living coccolithophores in ocean waters. In: Winter A, Siesser WG (eds) Coccolithophores. Cambridge University Press, pp 161–177
Young JR (1998) Neogene. In: Bown PR (ed) Calcareous nannofossil biostratigraphy. Kluwer Academic Publishers, pp 225–265
Young JR, Bown PR (1997) Cenozoic calcareous nannoplankton classification. J Nannoplankton Res 19: 36–47
Young JR, Didymus JM, Bown PR, Prins B, Mann S (1992) Crystal assembly and phylogenetic evolution in heterococcoliths. Nature 356: 516–518
Young JR, Bown PR, Burnett JA (1994) The Haptophytes: Palaeontological perspectives. In: Green JC, Leadbeater BSC (eds) The Haptophyte Algae. The Systematics Association Special Volume No. 51, pp 379–392
Zachos JC, Stott LD, Lohmann KC (1994) Evolution of early Cenozoic temperatures. Paleoceanography 9: 353–387
Zachos JC, Pagani M, Sloan L, Thomas E, Billups K (2001) Trends, rhythms, and aberrations in global climate 65 Ma to present. Science 292: 696–693
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2004 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Bown, P.R., Lees, J.A., Young, J.R. (2004). Calcareous nannoplankton evolution and diversity through time. In: Thierstein, H.R., Young, J.R. (eds) Coccolithophores. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-06278-4_18
Download citation
DOI: https://doi.org/10.1007/978-3-662-06278-4_18
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-06016-8
Online ISBN: 978-3-662-06278-4
eBook Packages: Springer Book Archive