Vegetation and climate development on the North American Atlantic Coastal Plain from 33 to 13 million years ago (IODP Expedition 313)

Abstract

Abstract. We have investigated the palynology of sediment cores from Sites M0027 and M0029 of IODP Expedition 313 on the New Jersey shallow shelf, east coast of North America, spanning an age range of 33 to 13 million years before present. Additionally, a pollen assemblage from the Pleistocene was examined. The palynological results were statistically analyzed and complemented with pollen-based quantitative climate reconstructions. Transport-related bias of the pollen assemblages was identified via analysis of the ratio of terrestrial to marine palynomorphs, and considered when interpreting palaeovegetation and palaeoclimate from the pollen data. Results indicate that from the early Oligocene to the middle Miocene, the hinterland vegetation of the New Jersey shelf was characterized by oak-hickory forests in the lowlands and conifer-dominated vegetation in the highlands. The Oligocene witnessed several expansions of conifer forest, probably related to cooling events. The pollen-based climate data imply an increase in annual temperatures from ~12 °C to more than 15 °C during the Oligocene. The Mi-1 cooling event at the onset of the Miocene is reflected by an expansion of conifers and an annual temperature decrease by almost 3 °C, from 15 °C to 12.5 °C around 23 million years before present. Particularly low annual temperatures are also recorded for an interval around ~20 million years before present, which probably reflects the Mi-1aa cooling event. Generally, the Miocene ecosystem and climate conditions were very similar to those of the Oligocene in the hinterland of the New Jersey shelf. Miocene grasslands, as known from other areas in the USA during that time period, are not evident for the hinterland of the New Jersey shelf. Surprisingly, the palaeovegetation data for the hinterland of the New Jersey shelf do not show extraordinary changes during the Mid-Miocene climatic optimum at ~15 million years before present, except for a minor increase in deciduous-evergreen mixed forest taxa and a decrease in swamp forest taxa. Pollen-based annual temperature reconstructions show average annual temperatures of ~14 °C during the Mid-Miocene climatic optimum. We conclude that vegetation and regional climate in the hinterland of the New Jersey shelf did not react as sensitively to Oligocene and Miocene climate changes as other regions in North America or Europe. An additional explanation for the relatively low regional temperatures reconstructed for the Mid-Miocene climatic optimum could be an uplift of the Appalachian Mountains during the Miocene. The Pleistocene pollen assemblage probably derives from the Marine Isotope Chron 7 or 5e and shows climate conditions similar to present-day.

Southward shift of the Intertropical Convergence Zone due to Northern Hemisphere cooling at the Oligocene-Miocene boundary

“…This result is completely opposite to the picture of the cryosphere depicted in the literature; i.e., a build-up of Antarctic ice sheets reaching the present-day volume or larger, but with an ice-free Arctic (Zachos et al, 2001;Pekar and DeConto, 2006;Liebrand et al, 2011;Mawbey and Lear, 2013). Terrestrial pollen data from Denmark (Śliwińska et al, 2014), northeastern Tibet (Miao et al, 2013), and the North American Atlantic coastal plain (Kotthoff et al, 2013) support our interpretation; they show the sudden and brief expansion of conifer forests during the Mi-1 event, indicating cooling of 2-4 °C in the NH highmiddle latitude regions. This supporting evidence, with our own results, calls for a forcing mechanism that was able to drive the significant NH cooling during this episode.…”

Reconstrucción paleoflorística a partir de los conjuntos palinológicos recuperados de los lacustres Villa Alegría y Cerro Prieto en el Valle de Tehuacán-Cuicatlán, Puebla y Oaxaca

“…Este mismo autor observó una aberración climática para este periodo en el límite Eoceno-Oligoceno, hace unos 34 millones de años aproximadamente, donde se incrementó la placa de hielo continental de la Antártida y las temperaturas decayeron. Kotthoff et al, (2013) recuperaron palinomorfos del lecho marino de la costa este de Estados Unidos en New Jersey y encontraron que para finales del Eoceno los conjuntos palinológicos contenían altos porcentajes de polen bisacado el cual corresponde a bosques de coníferas e indicaron que la temperatura media anual decreció aproximadamente 3° C en la transición Eoceno-Oligoceno.…”

“…Estas condiciones climáticas adversas aceleraron las tasas de recambio y especiación en ciertos grupos, así como la extinción de otros. Kotthoff et al, (2013) basándose en los conjuntos paleopalinológicos recuperados de sedimentos marinos de las costas de New Jersey, dedujeron que hace unos 23.4 millones de años las temperaturas eran mucho más cálidas y que estas disminuyeron entre 3 y 4° C; como consecuencia, se observó una expansión de los bosques de coníferas, reflejado en los altos porcentajes de polen bisacado recuperado de dichos sedimentos. (Zachos et al, 2001).…”