An Astronomically-tuned High Resolution Benthic Isotope Stratigraphy for the Late Paleocene and Early Eocene

古新世晚期至始新世早期（~58 ~ 52 Mya）是地球气候变化最活跃的时期之一。s过去。它的特点是一个渐进的长期变暖趋势，在过去9000万年最温暖的条件下达到顶峰，始新世早期气候最佳期 然而，最近的调查发现，长期变暖趋势被几个短暂的（短暂的）变暖事件（持续时间为数万年）打断，这些事件被称为高温或始新世热最大值。 这些事件，其中包括极端的古新世-始新世热极大期（PETM，~56 Mya），被认为有一个共同的起源，可能涉及碳循环反馈放大的轨道强迫。 其他提出的驱动机制，特别是对于PETM，包括火山释气和/或海洋甲烷水合物的分解。 为了评估PETM和其他热极大值是否由轨道或其他强迫触发，我们打算建立这些事件与长期背景变化的时间关系（即，周期性）的气候和碳循环。为此，我们将利用从南大西洋回收的深海岩心，构建第一个高分辨率、天文调谐的底栖有孔虫稳定碳和氧同位素时间序列，时间约为5-6百万年。古新世上部-始新世下部的一段。 这些和其他记录将使我们能够建立相对的时间和阶段的热最大的碳循环中的偏移，从而提供定量评估气候的性质的限制？气候变暖期间的碳循环耦合。 除了这一应用外，天文调谐同位素时间序列将作为标准同位素参考剖面，所有其他古新世和早始新世深海序列都可以通过它进行比较。 在这种能力下，将有可能使用碳同位素将海洋沉积剖面的片段与我们的调谐记录相关联和校准，从而大大提高年龄模型的准确性。 这将有助于将天文校准转移到具有特殊磁性地层学的部分，从而转移到地磁极性时标。

TOWARD AN ASTRONOMICALLY-TUNED HIGH-RESOLUTION BENTHIC ISOTOPE STRATIGRAPHY FOR THE PALEOCENE AND EARLY EOCENEJAMES ZACHOS, UNIVERSITY OF CALIFORNIA, SANTA CRUZEAR-0959117ABSTRACTThe late Paleocene to early Eocene (~58 to 52 Mya) represents one of the most climatically dynamic periods of Earth?s past. It is characterized by a gradual long warming trend that culminates in the warmest conditions of the last 90 m.y., the Early Eocene Climatic Optimum. Recent investigations, however, have found that the long-term warming trend was punctuated by several short-lived (transient) warming events (tens of thousands of years in duration), referred to as hyperthermals or Eocene thermal maxima. These events, which include the extreme Paleocene-Eocene Thermal Maximum (PETM, ~56 Mya), are thought to have a common origin, possibly involving orbital forcing amplified by carbon cycle feedbacks. Other proposed driving mechanisms, particularly for the PETM, include volcanic outgassing and/or the decomposition of marine methane hydrates. To assess whether the PETM and other thermal maxima were triggered by orbital or other forcing, we intend to establish the temporal relationship of these events to the long-term background variability (i.e., periodicity) in climate and the cabon cycle. To this end, utilizing a deep sea core recovered from the south Atlantic, we will construct the first high-resolution, astronomically-tuned benthic foraminiferal stable carbon and oxygen isotope time series for a ~5-6 m.y. segment of the upper Paleocene-lower Eocene. These and other records will allow us to establish the relative timing and phasing of the thermal maxima to excursions in the carbon cycle, thus providing constraints for quantitatively evaluating the nature of climate ? carbon cycle coupling during periods of warming. In addition to this application, the astronomically-tuned isotope time-series will serve as a standard isotope reference section by which all other Paleocene and early Eocene deep-sea sequences can be compared. In this capacity, it will be possible to use the carbon isotopes to correlate and calibrate segments of marine sedimentary sections to our tuned record, thereby significantly improving the accuracy of age models. This will facilitate transfer of the astronomical calibrations to sections with exceptional magnetostratigraphy, and thus the geomagnetic polarity time-scale.