Marine and terrestrial environmental changes in NW Europe preceding carbon release at the Paleocene-Eocene transition

作者：Kender Sev^*; Stephenson Michael H; Riding James B; Leng Melanie J; Knox Robert W O' B; Peck Victoria L; Kendrick Christopher P; Ellis Michael A; Vane Christopher H; Jamieson Rachel

来源：Earth and Planetary Science Letters, 2012, 353: 108-120.

DOI：10.1016/j.epsl.2012.08.011

• Paleocene-Eocene boundary
• PETM
• carbon isotope excursion
• paleoecology
• paleoceanography
• North Sea

Environmental changes associated with the Paleocene-Eocene thermal maximum (PETM, similar to 56 Ma) have not yet been documented in detail from the North Sea Basin. Located within proximity to the North Atlantic igneous province (NAIP), the Kilda Basin, and the northern rain belt (paleolatitude 54 degrees N) during the PETM, this is a critical region for testing proposed triggers of atmospheric carbon release that may have caused the global negative carbon isotope excursion (CIE) in marine and terrestrial environments. The CIE onset is identified from organic matter delta C-13 in exceptional detail within a highly expanded sedimentary sequence. Pollen and spore assemblages analysed in the same samples for the first time allow a reconstruction of possible changes to vegetation on the surrounding landmass. Multiproxy palynological, geochemical, and sedimentologic records demonstrate enhanced halocline stratification and terrigenous deposition well before (10(3) yrs) the CIE, interpreted as due to either tectonic uplift possibly from a nearby magmatic intrusion, or increased precipitation and fluvial runoff possibly from an enhanced hydrologic cycle. Stratification and terrigenous deposition increased further at the onset and within the earliest CIE which, coupled with evidence for sea level rise, may be interpreted as resulting from an increase in precipitation over NW Europe consistent with an enhanced hydrologic cycle in response to global warming during the PETM. Palynological evidence indicates a flora dominated by pollen from coastal swamp conifers before the CIE was abruptly replaced with a more diverse assemblage of generalist species including pollen similar to modern alder, fern, and fungal spores. This may have resulted from flooding of coastal areas due to relative sea level rise, and/or ecologic changes forced by climate. A shift towards more diverse angiosperm and pteridophyte vegetation within the early CIE, including pollen similar to modern hickory, documents a long term change to regional vegetation.

• 出版日期2012-11-1
• 单位British Antarctic Survey